Suppression of Cold Weather Events over High-Latitude Continents in Warm Climates
Recent studies, using Lagrangian single-column atmospheric models, have proposed that in warmer climates more low clouds would form asmaritime airmasses advect intoNorthernHemisphere high-latitude continental interiors during winter (DJF). This increase in low cloud amount and optical thickness coul...
| Main Authors: | , , |
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| Other Authors: | |
| Format: | Article |
| Language: | English |
| Published: |
American Meteorological Society
2020
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| Online Access: | https://hdl.handle.net/1721.1/125777 |