On September 28, 2018, the cargo ship Venta Maersk docks in St. Petersburg, Russia, more than a month after departing from Vladivostok on the other side of the country. The successful traversal of the Russian Arctic was a landmark moment for the international shipping industry, as well as a sobering reminder of the extent to which the Earth's ice caps had melted.
The search for a fast way to move cargo from one end of Eurasia to the other by sea had begun centuries ago, and was a major driver of European exploration of North America. Until the 2000s, the fastest means of making the journey was to go around South Asia and reach Europe via the Suez Canal. As climate change led to a decrease in ice around the North Pole, however, opportunities arose to for shipping companies to use waters that were previously impossible to navigate.
The Venta was not the first ship to make the journey through the Russian Arctic, and it needed assistance from an icebreaker for several days. The Northern Sea Route, as it is commonly called, is still not a regular shipping lane, and it is only usable by "ice-class" ships like the Venta. Nonetheless, the Venta's journey, and shipping companies' recent investment in building more vessels capable of repeating it, signal that climatologists and businesspeople alike believe it’s a safe bet that Arctic ice will continue to melt.
READ MORE: Climate Change History
Early expeditions Edit
Before the Little Ice Age (late Middle Ages to the 19th century), Norwegian Vikings sailed as far north and west as Ellesmere Island, Skraeling Island and Ruin Island for hunting expeditions and trading with the Inuit and people of the Dorset culture who already inhabited the region.  Between the end of the 15th century and the 20th century, colonial powers from Europe dispatched explorers in an attempt to discover a commercial sea route north and west around North America. The Northwest Passage represented a new route to the established trading nations of Asia.
England called the hypothetical northern route the "Northwest Passage." The desire to establish such a route motivated much of the European exploration of both coasts of North America, also known as the New World. When it became apparent that there was no route through the heart of the continent, attention turned to the possibility of a passage through northern waters. There was a lack of scientific knowledge about conditions for instance, some people believed that seawater was incapable of freezing. (As late as the mid-18th century, Captain James Cook had reported that Antarctic icebergs had yielded fresh water, seemingly confirming the hypothesis). Explorers thought that an open water route close to the North Pole must exist.  The belief that a route lay to the far north persisted for several centuries and led to numerous expeditions into the Arctic. Many ended in disaster, including that by Sir John Franklin in 1845. While searching for him the McClure Arctic Expedition discovered the Northwest Passage in 1850.
In 1906, the Norwegian explorer Roald Amundsen was the first to complete the passage solely by ship, from Greenland to Alaska in the sloop Gjøa.  Since that date, several fortified ships have made the journey.
From east to west, the direction of most early exploration attempts, expeditions entered the passage from the Atlantic Ocean via the Davis Strait and through Baffin Bay, both of which are in Canada. Five to seven routes have been taken through the Canadian Arctic Archipelago, via the McClure Strait, Dease Strait, and the Prince of Wales Strait, but not all of them are suitable for larger ships.   From there ships passed through westward through the Beaufort Sea and the Chukchi Sea, and then southwards through the Bering Strait (separating Russia and Alaska), into the Pacific Ocean.
Potential as a shipping lane Edit
In the 21st century, major changes to the ice pack due to climate change have stirred speculation that the passage may become clear enough of ice to permit safe commercial shipping for at least part of the year. On August 21, 2007, the Northwest Passage became open to ships without the need of an icebreaker. According to Nalan Koc of the Norwegian Polar Institute, this was the first time the Passage has been clear since they began keeping records in 1972.   The Northwest Passage opened again on August 25, 2008.  It is usually reported in mainstream media that ocean thawing will open up the Northwest Passage (and the Northern Sea Route) for various kind of ships, making it possible to sail around the Arctic ice cap  and possibly cutting thousands of miles off shipping routes. Warning that the NASA satellite images suggested that the Arctic had entered a "death spiral" caused by climate change, Professor Mark Serreze, a sea ice specialist at the U.S. National Snow and Ice Data Center (NSIDC) said: "The passages are open. It's a historic event. We are going to see this more and more as the years go by."   
However, some thick sections of ice will remain hard to melt in the shorter term. Drifting and persistence of large chunks of ice, especially in springtime, can be problematic as they can clog entire straits or severely damage a ship's hull. Cargo routes may thus be slow and uncertain, depending on prevailing conditions and the ability to predict them. Because much containerized traffic operates in a just-in-time mode (which does not tolerate delays well) and because of the relative isolation of the passage (which impedes shipping companies from optimizing their operations by grouping multiple stopovers on the same itinerary), the Northwest Passage and other Arctic routes are not always seen as promising shipping lanes by industry insiders, at least for the time being.  The uncertainty related to physical damage to ships is also thought to translate into higher insurance premiums,  especially because of the technical challenges posed by Arctic navigation (as of 2014, only 12 percent of Canada's Arctic waters have been charted to modern standards). 
The Beluga group of Bremen, Germany, sent the first Western commercial vessels through the Northern Sea Route (Northeast Passage) in 2009.  Canada's Prime Minister Stephen Harper announced that "ships entering the North-West passage should first report to his government." 
The first commercial cargo ship to have sailed through the Northwest Passage was SS Manhattan in August 1969.   SS Manhattan, of 115,000 deadweight tonnage, was the largest commercial vessel ever to navigate the Northwest Passage.
The largest passenger ship to navigate the Northwest Passage was the cruise liner Crystal Serenity of gross tonnage 69,000. Starting on August 10, 2016, the ship sailed from Vancouver to New York City with 1,500 passengers and crew, taking 28 days. 
In 2018, two of the freighters leaving Baffinland's port in the Milne Inlet, on Baffin Island's north shore, were bound for ports in Asia.  Those freighters did not sail west through the remainder of the Northwest Passage, they sailed east, rounded the tip of Greenland, and transitted Russia's Northern Sea Route.
The Northwest Passage includes three sections:
- East of Baffin Island: Baffin Bay between Greenland and Baffin Island to Lancaster Sound at the north end of Baffin Island, or
- West of Baffin Island (impractical): Through Hudson Strait south of Baffin Island, north through the Foxe Basin, west through the Fury and Hecla Strait, north to Lancaster Sound through the Gulf of Boothia and Prince Regent Inlet. The Fury and Hecla Strait is usually closed by ice.
- North: From Lancaster Sound west through the Parry Channel to the Prince of Wales Strait on the northwest side of Victoria Island. M'Clure Strait to the northwest is ice-filled southwest through the Prince of Wales Strait between Victoria Island and Banks Island might be passable, or
- South: From Lancaster Sound west past Prince Regent Inlet (basically a cul-de-sac but it may be possible to exit west through the Bellot Strait), past Somerset Island, south through Peel Sound between Somerset Island and Prince of Wales Island, either southwest through Victoria Strait (ice-choked), or directly south along the coast through Rae Strait and James Ross Strait and west through Simpson Strait south of King William Island (shallow) into Queen Maud Gulf, then west along the mainland coast south of Victoria Island.
Many attempts were made to find a salt water exit west from Hudson Bay, but the Fury and Hecla Strait in the far north is blocked by ice. The eastern entrance and main axis of the northwest passage, the Parry Channel, was found in 1819. The approach from the west through Bering Strait is impractical because of the need to sail around ice near Point Barrow. East of Point Barrow the coast is fairly clear in summer. This area was mapped in pieces from overland in 1821–1839. This leaves the large rectangle north of the coast, south of Parry Channel and east of Baffin Island. This area was mostly mapped in 1848–1854 by ships looking for Franklin's lost expedition. The first crossing was made by Amundsen in 1903–1905. He used a small ship and hugged the coast.
The International Hydrographic Organization defines the limits of the Northwestern Passages as follows: 
As a result of their westward explorations and their settlement of Greenland, the Vikings sailed as far north and west as Ellesmere Island, Skraeling Island for hunting expeditions and trading with Inuit groups. The subsequent arrival of the Little Ice Age is thought to have been one of the reasons that European seafaring into the Northwest Passage ceased until the late 15th century. 
Strait of Anián Edit
In 1539, Hernán Cortés commissioned Francisco de Ulloa to sail along the Baja California Peninsula on the western coast of North America. Ulloa concluded that the Gulf of California was the southernmost section of a strait supposedly linking the Pacific with the Gulf of Saint Lawrence. His voyage perpetuated the notion of the Island of California and saw the beginning of a search for the Strait of Anián.
The strait probably took its name from Ania, a Chinese province mentioned in a 1559 edition of Marco Polo's book it first appears on a map issued by Italian cartographer Giacomo Gastaldi about 1562. Five years later Bolognino Zaltieri issued a map showing a narrow and crooked Strait of Anian separating Asia from the Americas. The strait grew in European imagination as an easy sea lane linking Europe with the residence of Khagan (the Great Khan) in Cathay (northern China).
Cartographers and seamen tried to demonstrate its reality. Sir Francis Drake sought the western entrance in 1579. The Greek pilot Juan de Fuca, sailing from Acapulco (in Mexico) under the flag of the Spanish crown, claimed he had sailed the strait from the Pacific to the North Sea and back in 1592. The Spaniard Bartholomew de Fonte claimed to have sailed from Hudson Bay to the Pacific via the strait in 1640.
Northern Atlantic Edit
The first recorded attempt to discover the Northwest Passage was the east–west voyage of John Cabot in 1497, sent by Henry VII in search of a direct route to the Orient.  In 1524, Charles V sent Estêvão Gomes to find a northern Atlantic passage to the Spice Islands. An English expedition was launched in 1576 by Martin Frobisher, who took three trips west to what is now the Canadian Arctic in order to find the passage. Frobisher Bay, which he first charted, is named after him.
As part of another expedition, in July 1583 Sir Humphrey Gilbert, who had written a treatise on the discovery of the passage and was a backer of Frobisher, claimed the territory of Newfoundland for the English crown. On August 8, 1585, the English explorer John Davis entered Cumberland Sound, Baffin Island. 
The major rivers on the east coast were also explored in case they could lead to a transcontinental passage. Jacques Cartier's explorations of the Saint Lawrence River in 1535 were initiated in hope of finding a way through the continent. Cartier became persuaded that the St. Lawrence was the Passage when he found the way blocked by rapids at what is now Montreal, he was so certain that these rapids were all that was keeping him from China (in French, la Chine), that he named the rapids for China. Samuel de Champlain renamed them Sault Saint-Louis in 1611, but the name was changed to Lachine Rapids in the mid-19th century.
In 1602, George Weymouth became the first European to explore what would later be called Hudson Strait when he sailed Discovery 300 nautical miles (560 km) into the Strait. Weymouth's expedition to find the Northwest Passage was funded jointly by the British East India Company and the Muscovy Company.   Discovery was the same ship used by Henry Hudson on his final voyage.
John Knight, employed by the British East India Company and the Muscovy Company, set out in 1606 to follow up on Weymouth's discoveries and find the Northwest Passage. After his ship ran aground and was nearly crushed by ice, Knight disappeared while searching for a better anchorage. 
In 1609, Henry Hudson sailed up what is now called the Hudson River in search of the Passage encouraged by the saltiness of the water in the estuary, he reached present-day Albany, New York, before giving up. On September 14, 1609, Hudson entered the Tappan Zee while sailing upstream from New York Harbor. At first, Hudson believed the widening of the river indicated that he had found the Northwest Passage. He proceeded upstream as far as present-day Troy before concluding that no such strait existed there. He later explored the Arctic and Hudson Bay.
In 1611, while in James Bay, Hudson's crew mutinied. They set Hudson and his teenage son John, along with seven sick, infirm, or loyal crewmen, adrift in a small open boat. He was never seen again.  
A mission was sent out in 1612, again in Discovery, commanded by Sir Thomas Button to find Henry Hudson and continue through the Northwest Passage. After failing to find Hudson, and exploring the west coast of Hudson Bay, Button returned home due to illness in the crew. In 1614, William Gibbons attempted to find the Passage, but was turned back by ice. The next year, 1615, Robert Bylot, a survivor of Hudson's crew, returned to Hudson Strait in Discovery, but was turned back by ice.  Bylot tried again in 1616 with William Baffin. They sailed as far as Lancaster Sound and reached 77°45′ North latitude, a record which stood for 236 years, before being blocked by ice.
On May 9, 1619, under the auspices of King Christian IV of Denmark–Norway, Jens Munk set out with 65 men and the king's two ships, Einhörningen (Unicorn), a small frigate, and Lamprenen (Lamprey), a sloop, which were outfitted under his own supervision. His mission was to discover the Northwest Passage to the Indies and China. Munk penetrated Davis Strait as far north as 69°, found Frobisher Bay, and then spent almost a month fighting his way through Hudson Strait. In September 1619, he found the entrance to Hudson Bay and spent the winter near the mouth of the Churchill River. Cold, famine, and scurvy destroyed so many of his men that only he and two other men survived. With these men, he sailed for home with Lamprey on July 16, 1620, reaching Bergen, Norway, on September 20, 1620.
René-Robert Cavelier, Sieur de La Salle built the sailing ship, Le Griffon, in his quest to find the Northwest Passage via the upper Great Lakes. Le Griffon disappeared in 1679 on the return trip of her maiden voyage.  In the spring of 1682, La Salle made his famous voyage down the Mississippi River to the Gulf of Mexico. La Salle led an expedition from France in 1684 to establish a French colony on the Gulf of Mexico. He was murdered by his followers in 1687. 
Henry Ellis, born in Ireland, was part of a company aiming to discover the Northwest Passage in May 1746. After the difficult extinction of a fire on board the ship, he sailed to Greenland, where he traded goods with the Inuit peoples on July 8, 1746. He crossed to the town of Fort Nelson and spent the summer on the Hayes River. He renewed his efforts in June 1747, without success, before returning to England.
In 1772, the English fur-trader Samuel Hearne travelled overland northwest from Hudson Bay to the Arctic Ocean, thereby proving that there was no strait connecting Hudson Bay to the Pacific Ocean.
Northern Pacific Edit
Most Northwest Passage expeditions originated in Europe or on the east coast of North America, seeking to traverse the Passage in the westbound direction. Some progress was made in exploring the western reaches of the imagined passage.
In 1728 Vitus Bering, a Danish Navy officer in Russian service, used the strait first discovered by Semyon Dezhnyov in 1648 but later accredited to and named after Bering (the Bering Strait). He concluded that North America and Russia were separate land masses by sailing between them. In 1741 with Lieutenant Aleksei Chirikov, he explored seeking further lands beyond Siberia. While they were separated, Chirikov discovered several of the Aleutian Islands while Bering charted the Alaskan region. His ship was wrecked off the Kamchatka Peninsula, as many of his crew were disabled by scurvy.
The Spanish made several voyages to the northwest coast of North America during the late 18th century. Determining whether a Northwest Passage existed was one of the motives for their efforts. Among the voyages that involved careful searches for a Passage included the 1775 and 1779 voyages of Juan Francisco de la Bodega y Quadra. The journal of Francisco Antonio Mourelle, who served as Quadra's second in command in 1775, fell into English hands. It was translated and published in London, stimulating exploration.
Captain James Cook made use of the journal during his explorations of the region. In 1791 Alessandro Malaspina sailed to Yakutat Bay, Alaska, which was rumoured to be a Passage. In 1790 and 1791 Francisco de Eliza led several exploring voyages into the Strait of Juan de Fuca, searching for a possible Northwest Passage and finding the Strait of Georgia. To fully explore this new inland sea, an expedition under Dionisio Alcalá Galiano was sent in 1792. He was explicitly ordered to explore all channels that might turn out to be a Northwest Passage.
Cook and Vancouver Edit
In 1776, Captain James Cook was dispatched by the Admiralty in Great Britain on an expedition to explore the Passage. A 1745 act, when extended in 1775, promised a £20,000 prize for whoever discovered the passage. Initially the Admiralty had wanted Charles Clerke to lead the expedition, with Cook (in retirement following his exploits in the Pacific) acting as a consultant. However, Cook had researched Bering's expeditions, and the Admiralty ultimately placed their faith in the veteran explorer to lead, with Clerke accompanying him.
After journeying through the Pacific, to make an attempt from the west, Cook began at Nootka Sound in April 1778. He headed north along the coastline, charting the lands and searching for the regions sailed by the Russians 40 years previously. The Admiralty's orders had commanded the expedition to ignore all inlets and rivers until they reached a latitude of 65°N. Cook, however, failed to make any progress in sighting a Northwestern Passage.
Various officers on the expedition, including William Bligh, George Vancouver, and John Gore, thought the existence of a route was 'improbable'. Before reaching 65°N they found the coastline pushing them further south, but Gore convinced Cook to sail on into the Cook Inlet in the hope of finding the route. They continued to the limits of the Alaskan peninsula and the start of the 1,200 mi (1,900 km) chain of Aleutian Islands. Despite reaching 70°N, they encountered nothing but icebergs. 
From 1792 to 1794, the Vancouver Expedition (led by George Vancouver who had previously accompanied Cook) surveyed in detail all the passages from the Northwest Coast. He confirmed that there was no such passage south of the Bering Strait.  This conclusion was supported by the evidence of Alexander MacKenzie, who explored the Arctic and Pacific Oceans in 1793.
19th century Edit
In the first half of the 19th century, some parts of the Northwest Passage (north of the Bering Strait) were explored separately by many expeditions, including those by John Ross, Elisha Kent Kane, William Edward Parry, and James Clark Ross overland expeditions were also led by John Franklin, George Back, Peter Warren Dease, Thomas Simpson, and John Rae. In 1826 Frederick William Beechey explored the north coast of Alaska, discovering Point Barrow. 
Sir Robert McClure was credited with the discovery of the Northwest Passage in 1851 when he looked across McClure Strait from Banks Island and viewed Melville Island. However, this strait was not navigable to ships at that time. The only usable route linking the entrances of Lancaster Sound and Dolphin and Union Strait was discovered by John Rae in 1854.
Franklin expedition Edit
In 1845, a lavishly equipped two-ship expedition led by Sir John Franklin sailed to the Canadian Arctic to chart the last unknown swaths of the Northwest Passage. Confidence was high, as they estimated there was less than 500 km (310 mi) remaining of unexplored Arctic mainland coast. When the ships failed to return, relief expeditions and search parties explored the Canadian Arctic, which resulted in a thorough charting of the region, along with a possible passage. Many artifacts from the expedition were found over the next century and a half, including notes that the ships were ice-locked in 1846 near King William Island, about halfway through the passage, and unable to break free. Records showed Franklin died in 1847 and Captain Francis Rawdon Moira Crozier took over command. In 1848 the expedition abandoned the two ships and its members tried to escape south across the tundra by sledge. Although some of the crew may have survived into the early 1850s, no evidence has ever been found of any survivors. In 1853 explorer John Rae was told by local Inuit about the disastrous fate of Franklin's expedition, but his reports were not welcomed in Britain.
Starvation, exposure and scurvy all contributed to the men's deaths. In 1981 Owen Beattie, an anthropologist from the University of Alberta, examined remains from sites associated with the expedition.  This led to further investigations and the examination of tissue and bone from the frozen bodies of three seamen, John Torrington, William Braine and John Hartnell, exhumed from the permafrost of Beechey Island. Laboratory tests revealed high concentrations of lead in all three (the expedition carried 8,000 tins of food sealed with a lead-based solder).  Another researcher has suggested botulism caused deaths among crew members.  Evidence from 1996, that confirms reports first made by John Rae in 1854 based on Inuit accounts, suggests that the last of the crew may have resorted to cannibalism of deceased members in an effort to survive. 
McClure expedition Edit
During the search for Franklin, Commander Robert McClure and his crew in HMS Investigator traversed the Northwest Passage from west to east in the years 1850 to 1854, partly by ship and partly by sledge. McClure started out from England in December 1849, sailed the Atlantic Ocean south to Cape Horn and entered the Pacific Ocean. He sailed the Pacific north and passed through the Bering Strait, turning east at that point and reaching Banks Island.
McClure's ship was trapped in the ice for three winters near Banks Island, at the western end of Viscount Melville Sound. Finally McClure and his crew—who were by that time dying of starvation—were found by searchers who had travelled by sledge over the ice from a ship of Sir Edward Belcher's expedition. They rescued McClure and his crew, returning with them to Belcher's ships, which had entered the Sound from the east. McClure and his crew returned to England in 1854 on one of Belcher's ships. They were the first people known to circumnavigate the Americas and to discover and transit the Northwest Passage, albeit by ship and by sledge over the ice. (Both McClure and his ship were found by a party from HMS Resolute, one of Belcher's ships, so his sledge journey was relatively short.  )
This was an astonishing feat for that day and age, and McClure was knighted and promoted in rank. (He was made rear-admiral in 1867.) Both he and his crew also shared £10,000 awarded them by the British Parliament. In July 2010 Canadian archaeologists found his ship, HMS Investigator, fairly intact but sunk about 8 m (26 ft) below the surface.  
John Rae Edit
The expeditions by Franklin and McClure were in the tradition of British exploration: well-funded ship expeditions using modern technology, and usually including British Naval personnel. By contrast, John Rae was an employee of the Hudson's Bay Company, which operated a far-flung trade network and drove exploration of the Canadian North. They adopted a pragmatic approach and tended to be land-based. While Franklin and McClure tried to explore the passage by sea, Rae explored by land. He used dog sleds and techniques of surviving in the environment which he had learned from the native Inuit. The Franklin and McClure expeditions each employed hundreds of personnel and multiple ships. John Rae's expeditions included fewer than ten people and succeeded. Rae was also the explorer with the best safety record, having lost only one man in years of traversing Arctic lands. In 1854,  Rae returned to the cities with information from the Inuit about the disastrous fate of the Franklin expedition.
Amundsen expedition Edit
The first explorer to conquer the Northwest Passage solely by ship was the Norwegian explorer Roald Amundsen. In a three-year journey between 1903 and 1906, Amundsen explored the passage with a crew of six. Amundsen, who had sailed to escape creditors seeking to stop the expedition, completed the voyage in the converted 45 net register tonnage (4,500 cu ft or 130 m 3 ) herring boat Gjøa. Gjøa was much smaller than vessels used by other Arctic expeditions and had a shallow draft. Amundsen intended to hug the shore, live off the limited resources of the land and sea through which he was to travel, and had determined that he needed to have a tiny crew to make this work. (Trying to support much larger crews had contributed to the catastrophic failure of John Franklin's expedition fifty years previously). The ship's shallow draft was intended to help her traverse the shoals of the Arctic straits.
Amundsen set out from Kristiania (Oslo) in June 1903 and was west of the Boothia Peninsula by late September. Gjøa was put into a natural harbour on the south shore of King William Island by October 3 she was iced in. There the expedition remained for nearly two years, with the expedition members learning from the local Inuit people and undertaking measurements to determine the location of the North Magnetic Pole. The harbour, now known as Gjoa Haven, later developed as the only permanent settlement on the island.
After completing the Northwest Passage portion of this trip and having anchored near Herschel Island, Amundsen skied 800 kilometres (500 mi) to the city of Eagle, Alaska. He sent a telegram announcing his success and skied the return 800 kilometres (500 mi) to rejoin his companions.  Although his chosen east–west route, via the Rae Strait, contained young ice and thus was navigable, some of the waterways were extremely shallow (3 ft (0.91 m) deep), making the route commercially impractical.
Later expeditions Edit
The first traversal of the Northwest Passage via dog sled  was accomplished by Greenlander Knud Rasmussen while on the Fifth Thule Expedition (1921–1924). Rasmussen and two Greenland Inuit travelled from the Atlantic to the Pacific over the course of 16 months via dog sled. 
Canadian Royal Canadian Mounted Police officer Henry Larsen was the second to sail the passage, crossing west to east, leaving Vancouver on June 23, 1940 and arriving at Halifax on October 11, 1942. More than once on this trip, he was uncertain whether St. Roch, a Royal Canadian Mounted Police "ice-fortified" schooner, would survive the pressures of the sea ice. At one point, Larsen wondered "if we had come this far only to be crushed like a nut on a shoal and then buried by the ice." The ship and all but one of her crew survived the winter on Boothia Peninsula. Each of the men on the trip was awarded a medal by Canada's sovereign, King George VI, in recognition of this feat of Arctic navigation. 
Later in 1944, Larsen's return trip was far more swift than his first. He made the trip in 86 days to sail back from Halifax, Nova Scotia, to Vancouver, British Columbia.  He set a record for traversing the route in a single season. The ship, after extensive upgrades, followed a more northerly, partially uncharted route.
In 1954, HMCS Labrador  completed the east-to-west transit, under the command of Captain O.C.S. Robertson, conducting hydrographic soundings along the route. She was the first warship (and the first deep draft ship) to transit the Northwest Passage and the first warship to circumnavigate North America. In 1956, HMCS Labrador again completed the east-to-west transit, this time under the command of Captain T.C. Pullen.
On July 1, 1957, the United States Coast Guard Cutter Storis departed in company with USCGC Bramble and USCGC Spar to search for a deep-draft channel through the Arctic Ocean and to collect hydrographic information. The US Coast Guard Squadron was escorted through Bellot Strait and the Eastern Arctic by HMCS Labrador.  Upon her return to Greenland waters, Storis became the first U.S.-registered vessel to circumnavigate North America. Shortly after her return in late 1957, she was reassigned to her new home port of Kodiak, Alaska.
In 1960, USS Seadragon completed the first submarine transit of the Northwest Passage, heading east-to-west. 
In 1969, SS Manhattan made the passage, accompanied by the Canadian icebreakers CCGS John A. Macdonald and CCGS Louis S. St-Laurent. The U.S. Coast Guard icebreakers Northwind and Staten Island also sailed in support of the expedition.  
Manhattan was a specially reinforced supertanker sent to test the viability of the passage for the transport of oil. While Manhattan succeeded, the route was deemed not to be cost-effective. The United States built the Alaska Pipeline instead.
In June 1977, sailor Willy de Roos left Belgium to attempt the Northwest Passage in his 13.8 m (45 ft) steel yacht Williwaw. He reached the Bering Strait in September and after a stopover in Victoria, British Columbia, went on to round Cape Horn and sail back to Belgium, thus being the first sailor to circumnavigate the Americas entirely by ship. 
In 1981 as part of the Transglobe Expedition, Ranulph Fiennes and Charles R. Burton completed the Northwest Passage. They left Tuktoyaktuk on July 26, 1981, in the 18-foot (5.5 m) open Boston Whaler and reached Tanquary Fiord on August 31, 1981. Their journey was the first open-boat transit from west to east and covered around 3,000 miles (4,800 km 2,600 nmi), taking a route through Dolphin and Union Strait following the south coast of Victoria and King William islands, north to Resolute Bay via Franklin Strait and Peel Sound, around the south and east coasts of Devon Island, through Hell Gate and across Norwegian Bay to Eureka, Greely Bay and the head of Tanquary Fiord. Once they reached Tanquary Fiord, they had to trek 150 miles (240 km) via Lake Hazen to Alert before setting up their winter base camp.
In 1984, the commercial passenger vessel MV Explorer (which sank in the Antarctic Ocean in 2007) became the first cruise ship to navigate the Northwest Passage. 
In July 1986, Jeff MacInnis and Mike Beedell set out on an 18-foot (5.5 m) catamaran called Perception on a 100-day sail, west to east, through the Northwest Passage.  This pair was the first to sail the passage, although they had the benefit of doing so over a couple of summers. 
In July 1986, David Scott Cowper set out from England in a 12.8-metre (42 ft) lifeboat named Mabel El Holland, and survived three Arctic winters in the Northwest Passage before reaching the Bering Strait in August 1989. He continued around the world via the Cape of Good Hope to return to England on September 24, 1990. His was the first vessel to circumnavigate the world via the Northwest Passage. 
On July 1, 2000, the Royal Canadian Mounted Police patrol vessel Nadon, having assumed the name St Roch II, departed Vancouver on a "Voyage of Rediscovery." Nadon ' s mission was to circumnavigate North America via the Northwest Passage and the Panama Canal, recreating the epic voyage of her predecessor, St. Roch. The 22,000-mile (35,000 km) Voyage of Rediscovery was intended to raise awareness concerning St. Roch and kick off the fund-raising efforts necessary to ensure the continued preservation of St. Roch. The voyage was organized by the Vancouver Maritime Museum and supported by a variety of corporate sponsors and agencies of the Canadian government. Nadon is an aluminum, catamaran-hulled, high-speed patrol vessel. To make the voyage possible, she was escorted and supported by the Canadian Coast Guard icebreaker Simon Fraser. The Coast Guard vessel was chartered by the Voyage of Rediscovery and crewed by volunteers. Throughout the voyage, she provided a variety of necessary services, including provisions and spares, fuel and water, helicopter facilities, and ice escort she also conducted oceanographic research during the voyage. The Voyage of Rediscovery was completed in five and a half months, with Nadon reaching Vancouver on December 16, 2000.
On September 1, 2001, Northabout, an 14.3-metre (47 ft) aluminium sailboat with diesel engine,  built and captained by Jarlath Cunnane, completed the Northwest Passage east-to-west from Ireland to the Bering Strait. The voyage from the Atlantic to the Pacific was completed in 24 days. Cunnane cruised in Northabout in Canada for two years before returning to Ireland in 2005 via the Northeast Passage he completed the first east-to-west circumnavigation of the pole by a single sailboat. The Northeast Passage return along the coast of Russia was slower, starting in 2004, requiring an ice stop and winter over in Khatanga, Siberia. He returned to Ireland via the Norwegian coast in October 2005. On January 18, 2006, the Cruising Club of America awarded Jarlath Cunnane their Blue Water Medal, an award for "meritorious seamanship and adventure upon the sea displayed by amateur sailors of all nationalities." [ citation needed ]
On July 18, 2003, a father-and-son team, Richard and Andrew Wood, with Zoe Birchenough, sailed the yacht Norwegian Blue into the Bering Strait. Two months later she sailed into the Davis Strait to become the first British yacht to transit the Northwest Passage from west to east. She also became the only British vessel to complete the Northwest Passage in one season, as well as the only British sailing yacht to return from there to British waters. 
In 2006, a scheduled cruise liner (MS Bremen) successfully ran the Northwest Passage,  helped by satellite images telling the location of sea ice.
On May 19, 2007, a French sailor, Sébastien Roubinet, and one other crew member left Anchorage, Alaska, in Babouche, a 7.5-metre (25 ft) ice catamaran designed to sail on water and slide over ice. The goal was to navigate west to east through the Northwest Passage by sail only. Following a journey of more than 7,200 km (4,474 mi), Roubinet reached Greenland on September 9, 2007, thereby completing the first Northwest Passage voyage made in one season without engine. 
In April 2009, planetary scientist Pascal Lee and a team of four on the Northwest Passage Drive Expedition drove the HMP Okarian Humvee rover a record-setting 496 km (308 mi) on sea-ice from Kugluktuk to Cambridge Bay, Nunavut, the longest distance driven on sea-ice in a road vehicle. The HMP Okarian was being ferried from the North American mainland to the Haughton–Mars Project (HMP) Research Station on Devon Island, where it would be used as a simulator of future pressurized rovers for astronauts on the Moon and Mars. The HMP Okarian was eventually flown from Cambridge Bay to Resolute Bay in May 2009, and then driven again on sea-ice by Lee and a team of five from Resolute to the West coast of Devon Island in May 2010.   The HMP Okarian reached the HMP Research Station in July 2011. The Northwest Passage Drive Expedition is captured in the motion picture documentary film Passage To Mars (2016). 
In 2009, sea ice conditions were such that at least nine small vessels and two cruise ships completed the transit of the Northwest Passage. These trips included one by Eric Forsyth  on board the 42-foot (13 m) Westsail sailboat Fiona, a boat he built in the 1980s. Self-financed, Forsyth, a retired engineer from the Brookhaven National Laboratory, and winner of the Cruising Club of America's Blue Water Medal, sailed the Canadian Archipelago with sailor Joey Waits, airline captain Russ Roberts and carpenter David Wilson.  After successfully sailing the Passage, the 77-year-old Forsyth completed the circumnavigation of North America, returning to his home port on Long Island, New York.
Cameron Dueck and his crew aboard the 40-foot sailing yacht Silent Sound also transited in the summer of 2009. Their voyage began in Victoria, BC on June 6 and they arrived in Halifax on October 10.  Dueck wrote a book about the voyage called The New Northwest Passage.  
On September 9, 2010, Bear Grylls and a team of five completed a point-to-point navigation between Pond Inlet and Tuktoyaktuk in the Northwest Territories on a rigid inflatable boat (RIB). The expedition drew attention to how the effects of global warming made this journey possible and raised funds for the Global Angels charity.  
On August 30, 2012 Sailing yacht Billy Budd,  110 feet (34 m), an English SY, successfully completed the Northwest Passage in Nome, Alaska, while sailing a northern route never sailed by a sailing pleasure vessel before. After six cruising seasons in the Arctic (Greenland, Baffin Bay, Devon Island, Kane Basin, Lancaster Sound, Peel Sound, Regent Sound) and four seasons in the South (Antarctic Peninsula, Patagonia, Falkland Islands, South Georgia), SY Billy Budd, owned by and under the command of an Italian sporting enthusiast, Mariacristina Rapisardi.  Crewed by Marco Bonzanigo, five Italian friends, one Australian, one Dutch, one South African, and one New Zealander, it sailed through the Northwest Passage. The northernmost route was chosen. Billy Budd sailed through the Parry Channel, Viscount Melville Sound and Prince of Wales Strait, a channel 160 nautical miles (300 km 180 mi) long and 15 nautical miles (28 km 17 mi) wide which flows south into the Amundsen Gulf. During the passage Billy Budd – likely a first for a pleasure vessel – anchored in Winter Harbour in Melville Island, the very same site where almost 200 years ago Sir William Parry was blocked by ice and forced to winter.
On August 29, 2012, the Swedish yacht Belzebub II, a 31-foot (9.4 m) fibreglass cutter captained by Canadian Nicolas Peissel, Swede Edvin Buregren and Morgan Peissel, became the first sailboat in history to sail through McClure Strait, part of a journey of achieving the most northerly Northwest Passage.  Belzebub II departed Newfoundland following the coast of Greenland to Qaanaaq before tracking the sea ice to Grise Fiord, Canada's most northern community. From there the team continued through Parry Channel into McClure Strait and the Beaufort Sea, tracking the highest latitudes of 2012's record sea ice depletion before completing their Northwest Passage September 14, 2012. The expedition received extensive media coverage, including recognition by former U.S. Vice President Al Gore.   The accomplishment is recorded in the Polar Scott Institute's record of Northwest Passage Transits and recognized by the Explorers Club  and the Royal Canadian Geographic Society. 
At 18:45 GMT on September 18, 2012, Best Explorer, a steel cutter 15.17 metres (49.8 ft), skipper Nanni Acquarone, passing between the two Diomedes, was the first Italian sailboat to complete the Northwest Passage along the classical Amundsen route. Twenty-two Italian amateur sailors took part of the trip, in eight legs from Tromsø, Norway, to King Cove, Alaska, totalling 8,200 nautical miles (15,200 km 9,400 mi). Later in 2019 Best Explorer skippered again by Nanni Acquarone became the first Italian sailboat to circumnavigate the Arctic sailing north of Siberia from Petropavlovsk-Kamchatsky to Tromsø and the second ever to do it clockwise. 
Setting sail from Nome, Alaska, on August 18, 2012, and reaching Nuuk, Greenland, on September 12, 2012, The World became the largest passenger vessel to transit the Northwest Passage.   The ship, carrying 481 passengers, for 26 days and 4,800 nmi (8,900 km 5,500 mi) at sea, followed in the path of Captain Roald Amundsen. The World 's transit of the Northwest Passage was documented by National Geographic photographer Raul Touzon. 
In September 2013, MS Nordic Orion became the first commercial bulk carrier to transit the Northwest Passage.  She was carrying a cargo of 73,500 short tons (66,700 t) of coking coal from Port Metro Vancouver, Canada, to the Finnish Port of Pori, 15,000 short tons (14,000 t) more than would have been possible via the traditional Panama Canal route.   The Northwest Passage shortened the distance by 1,000 nautical miles (1,900 km 1,200 mi) compared to traditional route via the Panama Canal.  
In August and September 2016 a cruise ship was sailed through the Northwest Passage.  The ship Crystal Serenity, (with 1,000 passengers, and 600 crew) left Seward, Alaska, used Amundsen's route and reached New York on September 17. Tickets for the 32-day trip started at $22,000 and were quickly sold out.  The trip was repeated in 2017. In 2017 33 vessels made a complete transit, breaking the prior record of 20 in 2012. 
In September 2018, sailing yacht Infinity (a 36·6 m ketch) and her 22-person crew successfully sailed through the Northwest Passage.  This was part of their mission to plant the Flag of Earth on the remaining Arctic ice. Supported by the EarthToday initiative, this voyage was a symbol for future global collaboration against climate change. The Flag of Planet Earth was planted on September 21, 2018, the International Day of Peace. 
The Canadian government classifies the waters of the Northwest Passage in the Canadian Arctic Archipelago, as internal waters of Canada as per the United Nations Convention on the Law of the Sea and by the precedent in the drawing of baselines for other archipelagos, giving Canada the right to bar transit through these waters.  Some maritime nations, including the United States and some of the European Union, claim these waters to be an international strait, where foreign vessels have the right of "transit passage." In such a regime, Canada would have the right to enact fishing and environmental regulation, and fiscal and smuggling laws, as well as laws intended for the safety of shipping, but not the right to close the passage.   If the passage's deep waters become completely ice-free in summer months, they will be particularly enticing for supertankers that are too big to pass through the Panama Canal and must otherwise navigate around the tip of South America. 
The dispute between Canada and the United States arose in 1969 with the trip of the U.S. oil tanker SS Manhattan through the Arctic Archipelago. The prospect of more American traffic headed to the Prudhoe Bay Oil Field made the Canadian government realize that political action was required. 
In 1985, the U.S. Coast Guard icebreaker Polar Sea passed through from Greenland to Alaska the ship submitted to inspection by the Canadian Coast Guard before passing through, but the event infuriated the Canadian public and resulted in a diplomatic incident. The United States government, when asked by a Canadian reporter, indicated that they did not ask for permission as they insist that the waters were an international strait. The Canadian government issued a declaration in 1986 reaffirming Canadian rights to the waters. The United States refused to recognize the Canadian claim. In 1988 the governments of Canada and the United States signed an agreement, "Arctic Cooperation," that resolved the practical issue without solving the sovereignty questions. Under the law of the sea, ships engaged in transit passage are not permitted to engage in research. The agreement states that all U.S. Coast Guard and Navy vessels are engaged in research, and so would require permission from the Government of Canada to pass through. 
However, in late 2005, it was reported that U.S. nuclear submarines had travelled unannounced through Canadian Arctic waters, breaking the "Arctic Cooperation" agreement and sparking outrage in Canada. In his first news conference after the 2006 federal election, Prime Minister-designate Stephen Harper contested an earlier statement made by the U.S. ambassador that Arctic waters were international, stating the Canadian government's intention to enforce its sovereignty there. The allegations arose after the U.S. Navy released photographs of USS Charlotte surfaced at the North Pole.  
On April 9, 2006, Canada's Joint Task Force (North) declared that the Canadian Forces will no longer refer to the region as the Northwest Passage, but as the Canadian Internal Waters.  The declaration came after the successful completion of Operation Nunalivut (Inuktitut for "the land is ours"), which was an expedition into the region by five military patrols. 
In 2006 a report prepared by the staff of the Parliamentary Information and Research Service of Canada suggested that because of the September 11 attacks, the United States might be less interested in pursuing the international waterways claim in the interests of having a more secure North American perimeter.  This report was based on an earlier paper, The Northwest Passage Shipping Channel: Is Canada's Sovereignty Really Floating Away? by Andrea Charron, given to the 2004 Canadian Defence and Foreign Affairs Institute Symposium.  Later in 2006 former United States Ambassador to Canada, Paul Cellucci agreed with this position however, the succeeding ambassador, David Wilkins, stated that the Northwest Passage was in international waters. 
On July 9, 2007, Prime Minister Harper announced the establishment of a deep-water port in the far North. In the press release Harper said, "Canada has a choice when it comes to defending our sovereignty over the Arctic. We either use it or lose it. And make no mistake, this Government intends to use it. Because Canada's Arctic is central to our national identity as a northern nation. It is part of our history. And it represents the tremendous potential of our future." 
On July 10, 2007, Rear Admiral Timothy McGee of the U.S. Navy and Rear Admiral Brian Salerno of the U.S. Coast Guard announced that the United States would be increasing its ability to patrol the Arctic. 
In June 2019, the U.S. State Department spokesperson Morgan Ortagus said the United States "believes that Canada's claim of the Northwest Passage are internal waters of Canada as inconsistent with international law" despite historical precedent regarding archipelago baselines. 
In summer 2000, two Canadian ships took advantage of thinning summer ice cover on the Arctic Ocean to make the crossing.  It is thought that climate change is likely to open the passage for increasing periods, making it potentially attractive as a major shipping route. However, the passage through the Arctic Ocean would require significant investment in escort vessels and staging ports, and it would remain seasonal. Therefore, the Canadian commercial marine transport industry does not anticipate the route as a viable alternative to the Panama Canal within the next 10 to 20 years (as of 2004). 
On September 14, 2007, the European Space Agency (ESA) stated that ice loss that year had opened up the historically impassable passage, setting a new low of ice cover as seen in satellite measurements which went back to 1978. According to the Arctic Climate Impact Assessment, the latter part of the 20th century and the start of the 21st had seen marked shrinkage of ice cover. The extreme loss in 2007 rendered the passage "fully navigable."   However, the ESA study was based only on analysis of satellite images and could in practice not confirm anything about the actual navigation of the waters of the passage. ESA suggested the passage would be navigable "during reduced ice cover by multi-year ice pack" (namely sea ice surviving one or more summers) where previously any traverse of the route had to be undertaken during favourable seasonable climatic conditions or by specialist vessels or expeditions. The agency's report speculated that the conditions prevalent in 2007 had shown the passage may "open" sooner than expected.  An expedition in May 2008 reported that the passage was not yet continuously navigable even by an icebreaker and not yet ice-free. 
Scientists at a meeting of the American Geophysical Union on December 13, 2007, revealed that NASA satellites observing the western Arctic [ clarification needed ] showed a 16% decrease in cloud coverage during the summer of 2007 compared to 2006. This would have the effect of allowing more sunlight to penetrate Earth's atmosphere and warm the Arctic Ocean waters, thus melting sea ice and contributing to opening the Northwest Passage. 
In 2006 the cruise liner MS Bremen successfully ran the Northwest Passage,  helped by satellite images telling where sea ice was.
On November 28, 2008, the Canadian Coast Guard confirmed the first commercial ship sailed through the Northwest Passage. In September 2008, MV Camilla Desgagnés, owned by Desgagnés Transarctik Inc. and, along with the Arctic Cooperative, part of Nunavut Sealift and Supply Incorporated (NSSI),  transported cargo from Montreal to the hamlets of Cambridge Bay, Kugluktuk, Gjoa Haven, and Taloyoak. A member of the crew is reported to have claimed that "there was no ice whatsoever." Shipping from the east was to resume in the fall of 2009.  Although sealift is an annual feature of the Canadian Arctic this was the first time that the western communities had been serviced from the east. The western portion of the Canadian Arctic is normally supplied by Northern Transportation Company Limited (NTCL) from Hay River, and the eastern portion by NNSI and NTCL from Churchill and Montreal.  
In January 2010, the ongoing reduction in the Arctic sea ice led telecoms cable specialist Kodiak-Kenai Cable to propose the laying of a fibre-optic cable connecting London and Tokyo by way of the Northwest Passage, saying the proposed system would nearly cut in half the time it takes to send messages from the United Kingdom to Japan.
In September 2013, the first large ice-strengthened sea freighter, Nordic Orion, used the passage. 
In 2016 a new record was set when the cruise ship Crystal Serenity transited with 1,700 passengers and crew.  Crystal Serenity is the largest cruise ship to navigate the Northwest Passage. Starting on August 10, 2016, the ship sailed from Vancouver to New York City, taking 28 days for the journey.
Transfer of Pacific species to North Atlantic Edit
Scientists believe that reduced sea ice in the Northwest Passage has permitted some new species to migrate across the Arctic Ocean.  The gray whale Eschrichtius robustus has not been seen in the Atlantic since it was hunted to extinction there in the 18th century, but in May 2010, one such whale turned up in the Mediterranean. Scientists speculated the whale had followed its food sources through the Northwest Passage and simply kept on going.   
The plankton species Neodenticula seminae had not been recorded in the Atlantic for 800,000 years. However, it has become increasingly prevalent there. Again, scientists believe that it got there through the reopened Northwest Passage.  
In August 2010, two bowhead whales from West Greenland and Alaska respectively, entered the Northwest Passage from opposite directions and spent approximately 10 days in the same area. 
Icebreaker's cyclone encounter reveals faster sea ice declinePhoto: Joo-Hong Kim, Korea Polar Research Institute
In August 2016 a massive storm on par with a Category 2 hurricane churned in the Arctic Ocean. The cyclone led to the third-lowest sea ice extent ever recorded. But what made the Great Arctic Cyclone of 2016 particularly appealing to scientists was the proximity of the Korean icebreaker Araon.
For the first time ever, scientists were able to see exactly what happens to the ocean and sea ice when a cyclone hits. University of Alaska Fairbanks researchers and their international colleagues recently published a new study showing that sea ice declined 5.7 times faster than normal during the storm. They were also able to prove that the rapid decline was driven by cyclone-triggered processes within the ocean.
Lead author Xiangdong Zhang from the UAF International Arctic Research Center, said:
"Generally, when storms come in, they decrease sea ice, but scientists didn't understand what really caused it."
There was general speculation that sea ice declined solely from atmospheric processes melting ice from above. Zhang and his team proved this theory incomplete using "in-situ" observations from directly inside the cyclone. The measurements reflected things like air and ocean temperature, radiation, wind and ocean currents.
It was a stroke of good luck for science, and perhaps a bit nerve-racking for those onboard, that the icebreaker was in position to capture data from the cyclone. Usually ships try to avoid such storms, but Araon had just sailed into the middle of an ice-covered zone and was locked in an ice floe.
Thanks to the ship's position so close to the storm, Xiangdong and his team were able to explain that cyclone-related sea ice loss is primarily due to two physical ocean processes.
First, strong spinning winds force the surface water to move away from the cyclone. This draws deeper warm water to the surface. Despite this warm water upwelling, a small layer of cool water remains directly beneath the sea ice.
That's where a second process comes into play. The strong cyclone winds act like a blender, mixing the surface water.
Together, the warm water upwelling and the surface turbulence warm the entire upper ocean water column and melt the sea ice from below.
Although the August storm raged for only 10 days, there were lasting effects.
"It's not just the storm itself. It has lingering effects because of the enhanced ice-albedo feedback."
The enlarged patches of open water from the storm absorb more heat, which melts more sea ice, causing even more open water. From Aug. 13-22, the amount of sea ice in the entire Arctic Ocean declined by 230,000 square miles, an area more than twice the size of the state of Arizona.
Xiangdong is now working with a new computer model for the Department of Energy to evaluate whether climate change will lead to more Arctic cyclones. Previous research shows that over the past half-century, the number and intensity of cyclones in the Arctic have increased. Some of those storms, like the biggest Arctic cyclone on record in 2012, also led to record low sea ice extent.
Antarctic ice shelf risks collapse due to warm mountain winds
The Larsen C Ice Shelf is located on the Antarctic Peninsula, which currently experiences the highest surface melt rates across Antarctica. Melt rates have been increasing in response to strengthening circumpolar winds that result from ozone depletion and increasing greenhouse gas concentrations.
The study provides the first comprehensive explanation for the melt experienced across the ice shelf.
Strengthening circumpolar winds have brought more warm maritime air to the region and increased the frequency and strength of warm mountain wind events known as foehn over the east coast of the Antarctic Peninsula, where Larsen C is located. The research found foehn winds drive the highest melt rates and govern the variability of melt across the ice shelf.
Dr. Andrew Elvidge, a senior research associate in UEA's School of Environmental Sciences, led the research. He will present the findings today at the annual meeting of the European Geophysical Union.
"Our study has shown that the dominant control on Larsen C surface melt is the occurrence, strength and warmth of foehn winds, and that the most intense foehn-driven melt occurs in embayments, or inlets.
"From previous studies we know these regions are now prone to melt water ponding, which is the precursor to hydrofracture, when crevasses are driven open by the weight of water generated by surface melt. This is the mechanism believed to have caused the catastrophic collapses of the nearby Larsen A and B ice shelves in 1995 and 2002, respectively.
"Foehn-driven melt on Larsen C is likely to increase in the future, with further strengthening of the circumpolar winds expected due to increasing greenhouse gas concentations.
"The collapse of ice shelves causes the glaciers that previously fed them to speed up and drain directly into the ocean, which leads to sea level rise."
The research, with co-author Prof Ian Renfrew of UEA's School of Environmental Sciences and scientists from Utrecht University and the British Antarctic Survey, used measurements of the ice shelf and atmosphere gathered between November 2014 to June 2017, in conjunction with atmospheric model simulations.
According to their findings, the inlets of Larsen C experience the highest melt rates, and although foehn winds are seen just 15 percent of the time, they account for 45 percent of the surface melt.
"This region is one of the fastest-warming on Earth and currently experiences the highest surface melt rates across Antarctica.
"Further work with weather and climate models is needed to improve predictions of the timescales on which Larsen C will become vulnerable to atmosphere-driven collapse."
Stena Line reveals the names of the new Baltic Sea vesselsPhoto: Stena Line
The new ferries will add a further 30 per cent freight capacity and offer an attractive alternative way to travel on the Baltic Sea. After receiving close to 600 name suggestions from customers online the new names are - Stena Scandica and Stena Baltica.
In October Stena Line announced the strengthening of their Baltic Sea fleet with the deployment of two modern RoPax vessels on the route between Nynäshamn in Sweden and Ventspils in Latvia during 2021, which will add 30 per cent more lane metres freight capacity and offer a brand new modern onboard experience. The two modern RoPax vessels were built at the Italian shipyard Visentini in 2005 and have been operating on Stena Line&rsquos Irish Sea route between Belfast and Liverpool for the last 10 years, with the names Stena Lagan and Stena Mersey. Before they start operating on their new route in the Baltic Sea the two vessels will be modernised and lengthened by sister company Stena RoRo, as well as receive new names.
Johan Edelman, Trade Director Baltic Sea North, says:
&ldquoThe new vessel names connect with our Scandinavian heritage as well as the region where they will operate. They vessels will add a brand new modern onboard experience for both travel and freight customers on the Baltic Sea."
The first of the two vessels, Stena Scandica (ex. Stena Lagan) is currently undergoing a ground-breaking conversion at the Sedef Shipyard in Tuzla, Turkey. It will join the Stena Line fleet and start operating on the Nynäshamn-Ventspils route during the first quarter of 2021.
The second vessel, Stena Mersey, is still operating on the Irish Sea where it will be replaced by Stena Line&rsquos new E-flexer, Stena Embla, when it arrives from China in the new year. It will be modernised and lengthened during the spring at the same shipyard and will rejoin the fleet and start sailing on the Baltic Sea before the summer. She will inherit the classic Stena Line vessel name Stena Baltica.
The two vessels will be lengthened with a 36 metre mid-section after the conversion they will be 222 metres long and have a capacity of 200 cabins, 970 passengers and 2,875 freight lane meters plus the additional car deck adding another 30 per cent freight capacity on the route. To increase the loading efficiency, they will also be modified with drive through capabilities on two levels. The vessels will also be fitted with hybrid scrubbers.
Johan Edelman, Trade Director Baltic Sea North, says:
&ldquoWe have seen an increase in demand from our customers across the Baltic Sea region. We are now strengthening our position and customer offer further with new modern vessels, more capacity and an attractive onboard experience on both our routes to and from Latvia during 2021."
The Arctic Bureau
The Arctic is warming at twice the global annual average. Snow and ice are melting at an alarming rate which affects both local ecosystems as well as the global climate system.
The Arctic contains about a quarter of the world's undiscovered oil and gas reserves as well as vast mineral reserves. As the ice continues to melt, these untapped reserves will become more accessible.
The presence of undiscovered oil and gas, as well as new and emerging shipping routes, has led to an increase in tensions between the Arctic states as well attracted the interest of non-Arctic nations like China.
The melting ice cap is enabling more cargo ships to transverse the Northwest Passage and North Sea Route, slashing the time it takes to transport cargo between China and Europe
The Arctic region, with its unique set of cultures, landscapes and wildlife is the perfect destination for any traveller.
The Arctic region is home to around 4 million people and dozens of distinct Indigenous groups.
The idea behind the Bureau’s directory is to bring together all freelance journalists, photographers, podcasters and documentary film-makers interested in Arctic issues. The majority of individuals in the directory will be based in, or around, the Arctic and Subarctic regions.
If you are a commissioning editor, looking for a story from the Arctic, then the directory is a great way to find a local, or specialised journalist.
The health of the Arctic plays a critical role in the rest of the world’s well-being. This is why we encourage individuals from all over the globe to join our directory as long as they feel they can contribute to the conversation, for example, you could be based in India writing about the migration patterns of Arctic birds, or a Chinese journalist focusing on the country’s trade ambitions in the Arctic.
At the Arctic Bureau, we also want to promote a more environmentally conscious way of reporting from the region. We hope that by providing a directory of journalists, we can encourage editors to use local talent as much as possible.
We also aim to increase communication and collaboration between journalists working on Arctic projects. If you are interested in a cross-regional project, then feel free to pitch us your idea, and we will put you in touch with the relevant journalists, alternatively contact them directly below.
The Arctic region has become a geopolitical hotspot as nations vie for control of the region’s untapped resources and emerging trade routes, both of which are a result of rising temperatures caused by climate change. However, this global narrative often neglects the local perspectives of the region’s four million inhabitants. The Arctic is home to over thirty different indigenous peoples, each with their history and vision for the future and we want to help ensure that they are represented in the media’s coverage of the region. If you are a freelance journalist reporting on indigenous cultures, please get in touch at [email protected]
The Arctic Tour de France
The Arctic Race of Norway is the northernmost professional bike race in the world. The multi-day trip has been held since 2013. It is not only of great importance for Norwegian cycling, but also for the country and its people.
Werner Müller Schell visited Kjøllefjord in 2018
Kjøllefjord is ready for the big festival. The colourful, typically Scandinavian wooden houses are festively decorated Norwegian flags line the streets as people flock in droves towards the otherwise sleepy town centre. Crowds gather around the point where the town hall, post office and a specialty shop for fishing accessories converge. Barriers have been set up, a large target banner, stages and even several video screens. The small fishing village has been preparing for this day for weeks – and now it’s time for it to shine.
Not much happens here, around a thousand kilometres north of the Arctic Circle, where winters are long and dark and summers are short. Only 950 people live in Kjøllefjord, which is one of the northernmost places on the Norwegian mainland and is only a three-hour boat trip from the famous Nordkapp. Most of the inhabitants work in fishing, reindeer herding or seasonal tourism when the well-known Hurtigruten ships dock in the harbour. If you want to visit Kjøllefjord by land, only one road leads to the coastal village, which is sandwiched between huge granite rocks and the cold ocean. The next settlement after Mehamn is almost 40 kilometres away. In between: a virtually untouched, rugged rocky landscape that is only inhabited by thousands of reindeer.
Kjøllefjord marks end of the second stage of the professional bike race, which since its foundation in 2013 has developed into one of the largest sporting events in the north. Even Norway’s Prime Minister Erna Solberg is expected to arrive in Kjøllefjord by the afternoon. “That is exactly what is unique about our race. We also visit small towns in our region every year, ”says Knut-Eirik Dybdal. He is the managing director of the Arctic Race, which is organised by the creators of the Tour de France.
A flagship for the entire region
A professional bike race, a thousand kilometres north of the Arctic Circle – it was not easy to get here, admits Dybdal, the man who came up with the idea of an Arctic race. The race was conceived during the early 2000s when Norwegian cycling was experiencing an unprecedented upswing. It was a period when Kurt Asle Arvesen, Thor Hushovd, and later Edvald Boasson Hagen and Alexander Kristoff – Norwegian cycling professionals began to establish themselves as some of the best cyclists in the world producing some sensational performances at the Tour de France. At the time, the Tour des Fjords and the Tour of Norway were the two professional stage races in the country. Meanwhile the north – with its harsh weather conditions was not considered a viable cycling region.
This has been an issue that Nord-Norge, the Norwegian term for Northern Norway, has had to contend with throughout its history. Out of more than the 100 major sporting events held in Norway since the Second World War, only one took place in the northern third of the country: the 1990 Speed Skating Sprint World Championship in Tromsø. “We tried to get the Olympic Games and a European Football Championship together with Sweden – but that didn’t work out because, among other things, the necessary sports cities in our sparsely populated region would not have been used afterwards,” explains the race director. A bicycle race for him is the perfect solution to the problem: “You don’t have to build stadiums – the streets already exist. In addition, a stage race offers the opportunity to bridge the large distances between the places here, to show our great landscape and to bring people together. Kjøllefjord is the best example, ”said Dybdal.
On the day of the race almost every inhabitant of the small fishing village is on their feet. Long before the arrival of any cyclists, people gather around the video screens in the town centre to follow the race as it meanders through the Arctic landscape. Many of the Sami living in this region wear their colourful costumes for the festive occasion. There is also a barbecue on the wooden terraces and over 100 children race for bets at the Mini Arctic Race in the town centre. Even if cycling does not play a significant role in the everyday lives of Kjøllefjord’s inhabitants, today the village lives and breathes the sport.
It is the North’s enthusiasm for the sport that enabled Knut-Eirik Dybdal to convince the organisers of the 2011 Tour de France that this could work. It was also the year that Norwegian cycling was at an all time high with Thor Hushovd donning the world champion’s rainbow jersey, as he won two stages at the Tour de France. Hushvod is also an integral part of the Arctic Race’s history. Dybdal remembers his first phone call with Hushvod with a smile: “I told Thor about our idea of bringing the best cyclists in the world to Northern Norway. He probably thought I was crazy. But he still supported us. ” The Norwegian cycling legend would go on to win the first edition of the Arctic Race in 2013. He is now the race’s official brand ambassador.
Today, Hushovd is attending the race in Kjøllefjord as a spectator. Children ask him for autographs and selfies, he patiently answers the reporter’s questions. “The region here is certainly one of the most beautiful areas in the world – for this reason alone, the Arctic Race is a very special bike race. And there is also the enthusiasm of the people which gives the race a family-friendly feel, ”he explains. A total of eight teams from this year’s Tour de France tackle the four stages from Kirkenes to Alta. Among them are the French mountain king Warren Barguil, the Olympic gold medalist Jakob Fuglsang and the cycling cross world champion Mathieu Van der Poel.
A platform for Norway’s talent
The Norwegian cyclists are just as important for the local fans as the global stars. Local hero August Jensen in particular – who has so far been the only cyclist from the north to go professional – is the main focus of interest. The 26-year-old has participated in all six editions of the Arctic Race of Norway so far and, despite strong competition, was stage winner and second overall last year. Jensen is a symbol of what makes this stage race so special for Norwegians. For the local cycling professionals, it is one of the best opportunities to demonstrate their talent on the international stage. “When I was young, there was none of that – neither a race nor a professional from our region,” explains Jensen.
In Kjøllefjord, many of the spectators are willing him on. But unfortunately it is not his year. The day before, during the opening phase, a tire defect in the finals costs him valuable time. On the way to Kjøllefjord he has been in the favourites group for a long time, but a sudden gust of wind brings him down and he has to bury all hopes for a top position. A disappointed murmur ripples through the rows of spectators when Jensen is shown on the video screen with his tattered jersey. However, the mood quickly rises again – especially when the sounds of the TV helicopter can be heard over the fjord and the final stage begins.
Over the course of the 195 kilometres, the race has developed into one of the most exciting in the competition’s history: splintering into small groups, the peloton chases the finish line down into the fjord – as the stormy, cloud-covered weather adds to the atmosphere. In the end it is the American, Colin Joyce, who wins the final sprint . Third place goes to young Norwegian professional Markus Hoelgaard. For Hoelgaard, who ultimately won the Arctic Race 2018 young talent ranking, it is one of his best moments in his career. “We’re racing against some of the strongest teams in the world. It is one of the most important races of the year for us, ”he says happily at the finish. Norway’s Prime Minister Erna Solberg also arrived in time for the final. “This race is incredibly important for the north”, she states in front of the audience before referring to the promotional aspect the race has for the region: “The Arctic Race generates a lot of interest and, thanks to the fantastic pictures, makes our beautiful Norwegian landscape known to the whole world. “
The race undoubtedly serves as picture-postcard for the unique nature of the north – with northern lights, fjords cut deep into the granite cliffs and wide plains with roaming reindeer. A platform for Norwegian riders to showcase their talents. And a project that made the dream of hosting a major sporting event north of the Arctic Circle a reality in Northern Norway. With the race broadcasted in 160 countries, the creators of the Arctic Race of Norway can be content in the fact that it is has been a rip roaring success. But they are still not satisfied: in the future, race director Knut-Eirik Dybdal dreams of staging a race on the polar island of Spitsbergen, one of the northernmost inhabited areas in the world. “We are extremely enthusiastic here. We can, and want to, push the limits, ”says Dybdal. Having witnessed the enthusiasm for the race in the tranquil Kjøllefjord, it is hard not to believe him.
Russian president Dmitry Medvedev yesterday ordered five warships to join the search - now focused off the west coast of Africa - for the 3,988-ton vessel.
Mark Clark, of the UK's Maritime and Coastguard Agency, said: 'The ship contacted Dover Coastguard on July 28 and that was the last time anyone has heard from them.
'There didn't seem anything suspicious when contact was made. It could well be that a crew member had a gun put to his head by a hijacker when contact was made, but who knows?'
Viktor Matveev of Solchart Management, which owns the vessel, said: 'The entire staff of my company is working very hard to establish communication with the ship. Unfortunately, there is no information so far.
'My view is that it is most likely that the vessel has been hijacked.'
On lookout: Russian sailors are hunting for the ship crewed by fellow countrymen
Microplastics are affecting melt rates of snow and ice
Microplastics have reached the farthest corners of the Earth, including remote fjords and even the Mariana Trench, one of the deepest parts of the ocean. Recently, yet another distant area of our planet has been found to contain these pollutants: glaciers and ice sheets. An Eos article examines how microplastics create changes in these icy ecosystems, and underscores the importance of properly distinguishing them from another form of pollution in snow, black carbon.
In addition to the large plastic waste, such as water bottles and milk jugs, that ends up on remote beaches, many pieces of plastic get broken down into smaller and smaller pieces by ocean waters and wind. These tiny particles are microplastics, minute pieces of plastic that were either broken down over time or were small to begin with, such as fibers from clothing or beads in face washes.
How do microplastics find their way in and onto snow to begin with? Peter Deneen, a writer at Watershed Progressive who is not affiliated with the article, explained:
"Most often microplastics end up in snow via airborne deposition. Microplastics&helliptend to be lighter than dust particles and become airborne more easily&hellipThese particles, due to their shape, can remain airborne and gain enough altitude to circulate with large-scale weather and be transported [to] faraway places."
Jing Ming, one of the authors of the article, emphasized that airborne travel is one of the reasons why microplastics are so prevalent.
The article highlights the distinction between microplastics and black carbon, another form of pollution which also collects on snow. Black carbon particles come from the combustion of fossil fuels by humans as well as from natural sources such as forest fires. Because of their dark color, black carbon particles absorb sunlight and heat the surfaces they land on. When they are deposited on snow and ice, they increase melt rates. As a result of this melting, the planet's bright, reflective surfaces decrease in area. And as a result of that decrease, even more sunlight is absorbed by the surface, resulting in greater warming.
Currently, almost all studies of black carbon ignore the co-presence of microplastics in snow, which also have an effect on melt rates. Ming explained:
"Microplastics depositing in snow will last hundreds of years or even longer. They can absorb solar radiation and reduce surface albedo given they are not completely transparent but with colour." The authors emphasize that it is not just the colored microplastics which absorb sunlight and heat up, but more translucent plastics as well. Translucent plastics, which ordinarily would not absorb light, can wear, break down, or become scratched all of these processes increase their absorption levels.
As current measurements and instruments do not account for the presence of microplastics, their effect on melt rates can mistakenly be attributed to black carbon. Ming explained that, as a result, "the forcing of black carbon in snow may need to be reassessed owing to the coexistence of microplastics." In other words, the measured effect of black carbon on snow melt may be considerably different from the actual effect, due to the neglected presence of microplastics.
In order to begin sorting out the different impacts of microplastics and black carbon, the article suggests three simple changes. The first is to use glass bottles to collect field samples in order to avoid plastic contamination. The second is to filter melted snow samples in order to separate microplastic particles. And the third is to centrifuge (spin at a high speed) samples to separate microplastic particles, as they generally have a lower density than black carbon particles. Ming emphasized that "we should quickly set up a protocol to measure microplastics in snow, differentiate microplastics from black carbon and separate their individual roles in affecting snow."
Deneen highlighted another important consideration of microplastics in snow. Deneen, who is a former GlacierHub editor, explained:
"The thing about microplastics on snow/ice is that snow/ice are not what we would call a 'microplastics sink. Snow and ice melts and as it does, those particles are transported through a variety of ecosystems, contaminating riparian habitat, estuarian, and eventually marine."
As they reach these ecosystems, whether through snow melt or otherwise, microplastics pick up chemical contaminants and can disturb many forms of life: animals can ingest them, harming not only themselves, but also humans who eat them. Smaller invertebrates will consume microplastics, then be consumed by fish, and the plastic makes its way up the food chain until it arrives on a plate.
Many hands will be needed to tackle the broader issue of microplastic pollution. Deneen said:
"We need people, companies, and governments working at it from all sides to find alternative materials and shift the culture that has come to depend upon [plastics]."
He strongly emphasized the need for sufficient and substantial policy that imposes limits on plastic production and use, and that aims to clean up the already damaged terrains.
Microplastics affect an extremely wide range of ecosystems. As demonstrated by their presence in snow, microplastics affect each ecosystem in distinct ways, depending on the context and existence of other factors, such as black carbon. Understanding these differences is crucial to responding to the microplastics crisis. Battling plastics means addressing pollution not only in oceans and beaches, but on high mountain glaciers as well.
Early proposals in Panama Edit
The earliest record relating to a canal across the Isthmus of Panama was in 1534, when Charles V, Holy Roman Emperor and King of Spain, ordered a survey for a route through the Americas in order to ease the voyage for ships traveling between Spain and Peru. The Spanish were seeking to gain a military advantage over the Portuguese. 
In 1668, the English physician and philosopher Sir Thomas Browne speculated in his encyclopedic work, Pseudodoxia Epidemica, that "some Isthmus have been eaten through by the Sea, and others cut by the spade: And if the policy would permit, that of Panama in America were most worthy the attempt: it being but few miles over, and would open a shorter cut unto the East Indies and China". 
In 1788, American Thomas Jefferson, then Minister to France, suggested that the Spanish should build the canal, since they controlled the colonies where it would be built. He said that this would be a less treacherous route for ships than going around the southern tip of South America, and that tropical ocean currents would naturally widen the canal after construction.  During an expedition from 1788 to 1793, Alessandro Malaspina outlined plans for construction of a canal. 
Given the strategic location of Panama, and the potential of its narrow isthmus separating two great oceans, other trade links in the area were attempted over the years. The ill-fated Darien scheme was launched by the Kingdom of Scotland in 1698 to set up an overland trade route. Generally inhospitable conditions thwarted the effort, and it was abandoned in April 1700. 
Numerous canals were built in other countries in the late 18th and early 19th centuries. The success of the Erie Canal through central New York in the United States in the 1820s, and the collapse of the Spanish Empire in Latin America resulted in growing American interest in building an inter-oceanic canal. Beginning in 1826, US officials began negotiations with Gran Colombia (present-day Colombia, Venezuela, Ecuador, and Panama), hoping to gain a concession to build a canal. Jealous of their newly gained independence and fearing domination by the more powerful United States, president Simón Bolívar and New Granada officials declined American offers. After the collapse of Gran Colombia, New Granada remained unstable under constant government intrigue. [ citation needed ]
Great Britain attempted to develop a canal in 1843. According to the New-York Daily Tribune, August 24, 1843, the Barings of London and the Republic of New Granada entered into a contract for the construction of a canal across the Isthmus of Darien (Isthmus of Panama). They referred to it as the Atlantic and Pacific Canal, and it was a wholly British endeavor. Projected for completion in five years, the plan was never carried out. At nearly the same time, other ideas were floated, including a canal (and/or a railroad) across Mexico's Isthmus of Tehuantepec. That did not develop, either. 
In 1846, the Mallarino–Bidlack Treaty, negotiated between the US and New Granada, granted the United States transit rights and the right to intervene militarily in the isthmus. In 1848, the discovery of gold in California, on the West Coast of the United States, generated renewed interest in a canal crossing between the Atlantic and Pacific oceans. William H. Aspinwall, who had won the federal subsidy to build and operate the Pacific mail steamships at around the same time, benefited from the gold discovery. Aspinwall's route included steamship legs from New York City to Panama, and from Panama to California, with an overland portage through Panama. This route with an overland leg in Panama was soon frequently traveled, as it provided one of the fastest connections between San Francisco, California, and the East Coast cities, about 40 days' transit in total. Nearly all the gold that was shipped out of California went by the fast Panama route. Several new and larger paddle steamers were soon plying this new route, including private steamship lines owned by American entrepreneur Cornelius Vanderbilt that made use of an overland route through Nicaragua.  [ page needed ]
In 1850 the United States began construction of the Panama Railroad (now called the Panama Railway) to cross the isthmus it opened in 1855. This overland link became a vital piece of Western Hemisphere infrastructure, greatly facilitating trade. The later canal route was constructed parallel to it, as it had helped clear dense forests. [ citation needed ]
An all-water route between the oceans was still the goal. In 1855 William Kennish, a Manx-born engineer working for the United States government, surveyed the isthmus and issued a report on a route for a proposed Panama Canal.  His report was published as a book entitled The Practicability and Importance of a Ship Canal to Connect the Atlantic and Pacific Oceans.  [ page needed ]
In 1877, Armand Reclus, an officer with the French Navy, and Lucien Napoléon Bonaparte Wyse, both engineers, surveyed the route and published a French proposal for a canal.  [ page needed ] The French had achieved success in building the Suez Canal in the Mideast. While it was a lengthy project, they were encouraged to plan for a canal to cross the Panamanian isthmus. 
French construction attempts, 1881–1894 Edit
The first attempt to construct a canal through what was then Colombia's province of Panama began on January 1, 1881. The project was inspired by the diplomat Ferdinand de Lesseps, who was able to raise considerable funds in France as a result of the huge profits generated by his successful construction of the Suez Canal.  Although the Panama Canal needed to be only 40 percent as long as the Suez Canal, it was much more of an engineering challenge due to the combination of tropical rain forests, debilitating climate, the need for canal locks, and the lack of any ancient route to follow.
De Lesseps wanted a sea-level canal (like the Suez), but he visited the site only a few times, during the dry season which lasts only four months of the year.  His men were totally unprepared for the rainy season, during which the Chagres River, where the canal started, became a raging torrent, rising up to 10 m (35 ft). The dense jungle was alive with venomous snakes, insects, and spiders, but the worst challenges were yellow fever, malaria, and other tropical diseases, which killed thousands of workers by 1884, the death rate was over 200 per month.  Public health measures were ineffective because the role of the mosquito as a disease vector was then unknown. Conditions were downplayed in France to avoid recruitment problems,  but the high mortality rate made it difficult to maintain an experienced workforce.
Workers had to continually widen the main cut through the mountain at Culebra and reduce the angles of the slopes to minimize landslides into the canal.  Steam shovels were used in the construction of the canal, purchased from Bay City Industrial Works, a business owned by William L. Clements in Bay City, Michigan.  Bucket chain excavators manufactured by both Alphonse Couvreux and Wehyer & Richemond and Buette were also used.  Other mechanical and electrical equipment was limited in capabilities, and steel equipment rusted rapidly in the rainy climate. 
In France, de Lesseps kept the investment and supply of workers flowing long after it was obvious that the targets were not being met, but eventually the money ran out. The French effort went bankrupt in 1889 after reportedly spending US$287,000,000 an estimated 22,000 men died from disease and accidents, and the savings of 800,000 investors were lost.   Work was suspended on May 15, and in the ensuing scandal, known as the Panama affair, some of those deemed responsible were prosecuted, including Gustave Eiffel.  De Lesseps and his son Charles were found guilty of misappropriation of funds and sentenced to five years' imprisonment. This sentence was later overturned, and the father, at age 88, was never imprisoned. 
In 1894, a second French company, the Compagnie Nouvelle du Canal de Panama, was created to take over the project. A minimal workforce of a few thousand people was employed primarily to comply with the terms of the Colombian Panama Canal concession, to run the Panama Railroad, and to maintain the existing excavation and equipment in salable condition. The company sought a buyer for these assets, with an asking price of US$109,000,000. In the meantime, they continued with enough activity to maintain their franchise. Phillipe Bunau-Varilla, the French manager of the New Panama Canal Company, eventually managed to persuade de Lesseps that a lock-and-lake canal was more realistic than a sea-level canal. 
United States acquisition Edit
At this time, the President and the Senate of the United States were interested in establishing a canal across the isthmus, with some favoring a canal across Nicaragua and others advocating the purchase of the French interests in Panama. Bunau-Varilla, who was seeking American involvement, asked for $100 million, but accepted $40 million in the face of the Nicaraguan option. In June 1902, the US Senate voted in favor of the Spooner Act, to pursue the Panamanian option, provided the necessary rights could be obtained. 
On January 22, 1903, the Hay–Herrán Treaty was signed by United States Secretary of State John M. Hay and Colombian Chargé Dr. Tomás Herrán. For $10 million and an annual payment, it would have granted the United States a renewable lease in perpetuity from Colombia on the land proposed for the canal.  The treaty was ratified by the US Senate on March 14, 1903, but the Senate of Colombia did not ratify it. Bunau-Varilla told President Theodore Roosevelt and Hay of a possible revolt by Panamanian rebels who aimed to separate from Colombia, and hoped that the United States would support the rebels with US troops and money. [ citation needed ]
Roosevelt changed tactics, based in part on the Mallarino–Bidlack Treaty of 1846, and actively supported the separation of Panama from Colombia. Shortly after recognizing Panama, he signed a treaty with the new Panamanian government under terms similar to the Hay–Herrán Treaty. 
On November 2, 1903, US warships blocked sea lanes against possible Colombian troop movements en route to put down the Panama rebellion. Panama declared independence on November 3, 1903. The United States quickly recognized the new nation.  This happened so quickly that by the time the Colombian government in Bogotá launched a response to the Panamanian uprising US troops had already entered the rebelling province. It should also be stated that the Colombian troops dispatched to Panama were hastily assembled conscripts with little training. While these Conscripts may have been able to defeat the Panamanian rebels, they would not have been able to defeat the US army troops that were supporting the Panamanian rebels. The reason why an army of conscripts was sent was because that was the best response the Colombians could gather due to the fact that Colombia was still recovering from a civil war within Colombia that was between Liberals and Conservatives from October 1899 to November 1902 known as the “Thousand Days War.” With the US being fully aware of these conditions and even incorporating them into the planning of the Panama intervention as the US acted as an arbitrator between the two sides with the peace treaty that ended the “Thousand Days War” being signed on the USS Wisconsin on November 21, 1902. While in port the US also brought engineering teams to Panama, with the peace delegation, to begin planning for the canal's construction before the US had even gained the rights to build the canal. All these factors would result in the Colombians being unable to put down the Panamanian rebellion and expel the United States troops occupying what today is the independent nation of Panama. 
On November 6, 1903, Philippe Bunau-Varilla, as Panama's ambassador to the United States, signed the Hay–Bunau-Varilla Treaty, granting rights to the United States to build and indefinitely administer the Panama Canal Zone and its defenses. This is sometimes misinterpreted as the "99-year lease" because of misleading wording included in article 22 of the agreement.  Almost immediately, the treaty was condemned by many Panamanians as an infringement on their country's new national sovereignty.   This would later become a contentious diplomatic issue among Colombia, Panama, and the United States.
President Roosevelt famously stated, "I took the Isthmus, started the canal and then left Congress not to debate the canal, but to debate me." Several parties in the United States called this an act of war on Colombia: The New York Times described the support given by the United States to Bunau-Varilla as an "act of sordid conquest." [ citation needed ] The New York Evening Post called it a "vulgar and mercenary venture." [ citation needed ] The US maneuvers are often cited as the classic example of US gunboat diplomacy in Latin America, and the best illustration of what Roosevelt meant by the old African adage, "Speak softly and carry a big stick [and] you will go far." After the revolution in 1903, the Republic of Panama became a US protectorate until 1939. 
In 1904, the United States purchased the French equipment and excavations, including the Panama Railroad, for US$40 million, of which $30 million related to excavations completed, primarily in the Culebra Cut, valued at about $1.00 per cubic yard.  The United States also paid the new country of Panama $10 million and a $250,000 payment each following year.
In 1921, Colombia and the United States entered into the Thomson–Urrutia Treaty, in which the United States agreed to pay Colombia $25 million: $5 million upon ratification, and four-$5 million annual payments, and grant Colombia special privileges in the Canal Zone. In return, Colombia recognized Panama as an independent nation. 
MCA calls for seabird pollutant PIB reclassification - BBC News England
If approved she said it could affect the way the substance is discharged in the future.
The MCA is expected to present a paper to the IMO in either October or November.
The IMO is the United Nations agency responsible for the safety and security of shipping and the prevention of marine pollution by ships. It consists of 170 member states, of which the UK is one.
The organisation has confirmed a number of European countries, including the UK, have been investigating the discharge of "high viscosity products" by chemical tankers, including PIBs.
The application by the MCA is expected to be approved unless any of the member states lodges an objection.
The RSPB is planning its own campaign strategy on the matter and will give evidence to the government about PIBs at a meeting of the transport select committee in November.
It said the substance becomes "glue-like" in the sea, covering birds and restricting their movements and ability to feed "causing immobilisation, hypothermia, starvation and eventually death".
In August, the MCA said it had been unable to trace the vessel the contamination spill had come from and closed its investigation.
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