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Frozen Strait
Frozen Strait is a waterway in Nunavut just north of Hudson Bay between the Melville Peninsula to the north and Southampton Island to the south. It connects Repulse Bay to the west with Foxe Basin to the east. The strait is long, and 19 to 32 km (12 to 20 miles) wide. In 1615 Robert Bylot was blocked by ice at its east end. In 1742 Christopher Middleton reached the west end. He sailed north through Roes Welcome Sound to Repulse Bay. Seeing the strait ice-filled in August, it seemed clear that there was no passage so he gave the names Frozen Strait and Repulse Bay. In 1821 William Edward Parry passed the strait with no difficulty. Some have suggested that bowhead whales appear to migrate in the spring and fall through Roes Welcome Sound, but the possibility of migration through Frozen Strait cannot be ruled out. See also * Arctic oscillation * Maunder minimum * Great Frost of 1683–84 * Great Frost of 1709 * Little Ice Age * River Thames frost fairs The River Thames fros ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nunavut
Nunavut ( , ; iu, ᓄᓇᕗᑦ , ; ) is the largest and northernmost Provinces and territories of Canada#Territories, territory of Canada. It was separated officially from the Northwest Territories on April 1, 1999, via the ''Nunavut Act'' and the ''Nunavut Land Claims Agreement, Nunavut Land Claims Agreement Act'', which provided this territory to the Inuit for independent government. The boundaries had been drawn in 1993. The creation of Nunavut resulted in the territorial evolution of Canada, first major change to Canada's political map in half a century since the province of Newfoundland and Labrador, Newfoundland was admitted in 1949. Nunavut comprises a major portion of Northern Canada and most of the Arctic Archipelago. Its vast territory makes it the list of the largest country subdivisions by area, fifth-largest country subdivision in the world, as well as North America's second-largest (after Greenland). The capital Iqaluit (formerly Frobisher Bay), on Baffin Islan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bowhead Whales
The bowhead whale (''Balaena mysticetus'') is a species of baleen whale belonging to the family Balaenidae and the only living representative of the genus ''Balaena''. They are the only baleen whale endemic to the Arctic and subarctic waters, and are named after their characteristic massive triangular skull, which they use to break through Arctic ice. Other common names of the species are the Greenland right whale, Arctic whale, and Arviq in aboriginal languages (Inuktitut). American whalemen called them the steeple-top, polar whale, or Russian whale. Bowheads have the largest mouth of any animal representing almost one-third of the length of the body, the longest baleen plates with a maximum length of and may be the longest-lived mammals, with the ability to reach an age of more than 200 years. The bowhead was an early whaling target. Their population was severely reduced before a 1966 moratorium was passed to protect the species. Of the five stocks of bowhead populations, t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Thames Frost Fairs
The River Thames frost fairshttps://www.britishmuseum.org/research/collection_online/collection_object_details/collection_image_gallery.aspx?assetId=599805001&objectId=3199037&partId=1 Erra Paters Prophesy or Frost Faire 1684/3 were held on the tideway of the River Thames in London, England in some winters, starting at least as early as the late 7th century until the early 19th century. Most were held between the early 17th and early 19th centuries during the period known as the Little Ice Age, when the river froze over most frequently. During that time the British winter was more severe than it is now, and the river was wider and slower, further impeded by the 19 piers of the medieval Old London Bridge which were removed in 1831. Even at its peak, in the mid-17th century, the Thames in London froze less often than modern legend sometimes suggests, never exceeding about one year in ten except for four winters between 1649 and 1666. From 1400 until the removal of the medieval L ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Ice Age
The Little Ice Age (LIA) was a period of regional cooling, particularly pronounced in the North Atlantic region. It was not a true ice age of global extent. The term was introduced into scientific literature by François E. Matthes in 1939. Matthes described glaciers in the Sierra Nevada of California that he believed could not have survived the hypsithermal; his usage of "Little Ice Age" has been superseded by "Neoglaciation". The period has been conventionally defined as extending from the 16th to the 19th centuries, (noted in Grove 2004:4). but some experts prefer an alternative timespan from about 1300 to about 1850. The NASA Earth Observatory notes three particularly cold intervals. One began about 1650, another about 1770, and the last in 1850, all of which were separated by intervals of slight warming. The Intergovernmental Panel on Climate Change Third Assessment Report considered that the timing and the areas affected by the Little Ice Age suggested largely independent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Frost Of 1709
The Great Frost, as it was known in England, or ' ("The Great Winter"), as it was known in France, was an extraordinarily cold winter in Europe in 1708–1709,. and was the coldest European winter during the past 500 years. Notability William Derham recorded in Upminster, Great Britain, near London, a low of on the night of 5 January 1709, the lowest he had ever measured since he started taking readings in 1697. His contemporaries in the weather observation field in Europe likewise recorded lows down to . Derham wrote in '' Philosophical Transactions'': "I believe the Frost was greater (if not more universal also) than any other within the Memory of Man." During the Great Northern War, the Swedish invasion of Russia was notably weakened by the severe winter. Sudden winter storms and frosts killed thousands during the Swedish army's winter offensives, most notably during a single night away from camp that killed at least 2,000. Because the Russian troops were more prepared for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Frost Of 1683–84
The Great Frost of 1683–1684 was a frost across England, reported as the worst in its history. During the Frost, the surface of the River Thames was reported as frozen to the depth of . The Great Frost enabled one of the River Thames frost fairs. Entertainment on the frozen Thames as result of the Great Frost began the career of Chipperfield's Circus. A Great Frost Fair was also held in Leeds, when the River Aire froze solid for a month allowing a fair with an ox-roast and sports to take place, as described by Ralph Thoresby Ralph Thoresby (16 August 1658 – 16 October 1725) was an antiquarian, who was born in Leeds and is widely credited with being the first historian of that city. Besides being a merchant, he was a nonconformist, fellow of the Royal Society, di .... See also: Little Ice Age. References External links Contemporary reports of the 1683-1684 frost 1683 in England 1684 in England Cold waves in the United Kingdom {{disaster-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arctic Oscillation
The Arctic oscillation (AO) or Northern Annular Mode/Northern Hemisphere Annular Mode (NAM) is a weather phenomenon at the Arctic pole north of 20 degrees latitude. It is an important mode of climate variability for the Northern Hemisphere. The southern hemisphere analogue is called the Antarctic oscillation or Southern Annular Mode (SAM). The index varies over time with no particular periodicity, and is characterized by non-seasonal sea-level pressure anomalies of one sign in the Arctic, balanced by anomalies of opposite sign centered at about 37–45° N. The North Atlantic oscillation (NAO) is a close relative of the Arctic oscillation. There is debate over whether one or the other is more fundamentally representative of the atmosphere's dynamics. The NAO may be identified in a more physically meaningful way, which may carry more impact on measurable effects of changes in the atmosphere. Description The Arctic oscillation appears as a ringlike (or "annular") pattern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
William Edward Parry
Sir William Edward Parry (19 December 1790 – 8 July 1855) was an Royal Navy officer and explorer best known for his 1819–1820 expedition through the Parry Channel, probably the most successful in the long quest for the Northwest Passage, until it was finally negotiated by Roald Amundsen in 1906. In 1827, Parry attempted one of the earliest expeditions to the North Pole. He reached 82° 45' N, setting a record for human exploration Farthest North that stood for nearly five decades before being surpassed at 83° 20' N by Albert Hastings Markham in 1875. Early life Parry was born in Bath, Somerset, the son of Caleb Hillier Parry and Sarah Rigby. He was educated at King Edward's School. At the age of thirteen he joined the flagship of Admiral Sir William Cornwallis in the Channel fleet as a first-class volunteer, in 1806 became a midshipman, and in 1810 received promotion to the rank of lieutenant in the frigate ''Alexander'', which spent the ne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hudson Bay
Hudson Bay ( crj, text=ᐐᓂᐯᒄ, translit=Wînipekw; crl, text=ᐐᓂᐹᒄ, translit=Wînipâkw; iu, text=ᑲᖏᖅᓱᐊᓗᒃ ᐃᓗᐊ, translit=Kangiqsualuk ilua or iu, text=ᑕᓯᐅᔭᕐᔪᐊᖅ, translit=Tasiujarjuaq; french: baie d'Hudson), sometimes called Hudson's Bay (usually historically), is a large body of saltwater in northeastern Canada with a surface area of . It is located north of Ontario, west of Quebec, northeast of Manitoba and southeast of Nunavut, but politically entirely part of Nunavut. Although not geographically apparent, it is for climatic reasons considered to be a marginal sea of the Arctic Ocean. It Hudson Bay drainage basin, drains a very large area, about , that includes parts of southeastern Nunavut, Alberta, Saskatchewan, Ontario, Quebec, all of Manitoba, and parts of the U.S. states of North Dakota, South Dakota, Minnesota, and Montana. Hudson Bay's southern arm is called James Bay. The Cree language, Eastern Cree name for Hudson an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roes Welcome Sound
Roes Welcome Sound is a long channel at the northwest end of Hudson Bay in Kivalliq Region, Nunavut, Canada between the mainland on the west and Southampton Island on the east. It opens south into Hudson Bay. Its north end joins Repulse Bay which is connected east through Frozen Strait to Foxe Basin, thereby making Southampton Island an island. Wager Bay is a western branch. It is situated north of Marble Island. Roes Welcome Sound measures long, and wide. In 1613 it was reached by Thomas Button who called it 'Ne Ultra'. It is named after Sir Thomas Roe, friend and sponsor of explorer Luke Fox's 1631 Arctic voyage. Capt. Parry, trying to find the Northwest Passage during his 1821 voyage, wrote: "On an inspection of the charts, I think it will also appear probable that a communication will one day be found to exist between this inlet (Prince Regent's) and Hudson's Bay, either through the broad and unexplored channel called Sir Thomas Roe's Welcome, or through Repulse Bay, which h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Christopher Middleton (navigator)
Christopher Middleton ( – 12 February 1770) was a British navigator with the Hudson's Bay Company and Royal Navy officer. He was elected a Fellow of the Royal Society on 7 April 1737. Career Privateer in Queen Anne's War Middleton described serving aboard a privateer in Queen Anne's War. The war was fought between 1701 and 1713. Hudson's Bay Company service Middleton was appointed second mate of the ''Hannah'', in 1721, and appointed her captain in 1725. He eventually made 16 annual voyages on ships supplying Hudson Bay Company outposts. Middleton was a scientific sailor, and he methodically observed compass deviations, on his voyages. Hudson's Bay was close to the location of the North Magnetic Pole. Middleton published a paper, describing his observations, in the Royal Society's ''Philosophical Transactions''. Middleton's scientific endeavours earned him a Fellowship in the Royal Society. Northwest Passage On 5 March 1741, Middleton was appointed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
