Heat transport pathways into the Arctic and their connections to surface air temperatures
<p>Arctic amplification causes the meridional temperature gradient between middle and high latitudes to decrease. Through this decrease the large-scale circulation in the midlatitudes may change and therefore the meridional transport of heat and moisture increases. This in turn may increase Ar...
| Published in: | Atmospheric Chemistry and Physics |
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| Main Authors: | , |
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2019-03-01
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| Online Access: | https://www.atmos-chem-phys.net/19/3927/2019/acp-19-3927-2019.pdf |