Regional inputs to the Massachusetts Institute of Technology global circulation model: Chukchi Sea, Arctic Ocean, 1990-1992
The observed ongoing decline of summer sea ice coverage in the Arctic Ocean results, in part, from heat carried by ocean waters. This heat enters the Arctic Ocean by direct solar heating and by the transport of heat with flows from the Atlantic Ocean and Bering Sea. The warm waters from the Atlantic...
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| Format: | Dataset |
| Language: | unknown |
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Arctic Data Center
2017
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| Online Access: | https://doi.org/10.18739/A2DZ03253 |