Abstract
Abstract Canada’s IPY program funded seven marine projects spanning the North American Arctic. Work embraced oceanography, air-sea interactions, storm response, paleo-climate and trace-element chemistry. Notable findings are emerging. Conditions in the Beaufort were unusual in 2007, with very high air pressure bringing strong winds, rapid ice drift, thin winter ice, enhanced shelf-break upwelling and a maximum in freshwater retention in the Beaufort Gyre. A mapping of trace chemicals suggests that Arctic mid-depth circulation may also have reversed. Study of Canadian Arctic through-flow revealed a net annual seawater export of 44,000 cubic kilometres from the Arctic to Baffin Bay. Observations of sea ice, sustained through the IPY, affirmed that ice cover is the key attribute of Arctic seas, with wind as a potent agent in its variation. Surveys have shown that the anthropogenic decline in seawater alkalinity is aggravated in the Arctic by low temperature and low salinity resulting from ice melt. Careful experiments have revealed that Arctic phytoplankton growth is constrained by scarcity of dissolved iron where light levels are low. A manganese fingerprint in sediments has tracked changing sea level during the Ice Age. Sediment-core analysis has revealed the Arctic Oscillation as a dominant cause of long-period climate variations during the Holocene. One project has demonstrated how multi-tasked vessels can maintain a watch on Canada’s Arctic within a reliable affordable logistic framework, while a wave forecast model developed by another for the Beaufort is suitable for operational use.
Highlights
Canada’s International Polar Year (IPY) program funded seven marine projects spanning the North American Arctic
This paper describes Canadian Arctic marine science during the IPY
Since continental shelf underlies more than half the Arctic Ocean, understanding the physical and biogeochemical cycling of carbon on the shelves is tantamount to understanding Arctic marine carbon
Summary
The core of the Arctic is a deep ocean. Whereas maritime regions at lower latitude have climates distinctive for their moderation, the Arctic is different. Whereas land at the South Pole allows only the atmosphere to carry environmental influences to the highest Antarctic latitudes, the ocean is an active participant in the Arctic. Both atmospheric and oceanic exchanges mediate strong influences on the Arctic’s ice, ocean and ecosystem from the Pacific to Atlantic Oceans. The general circulation of the ocean is driven in part by that of the atmosphere (i.e., wind) and in part by pressure gradients that reflect differences in salinity as well as temperature of seawater. The paper demonstrates how Canadian work has advanced the prolonged international thrust to understand the Arctic Ocean and climate
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