A Satellite-Based Climatology of Wind-Induced Surface Temperature Anomalies for the Antarctic
It is well-known that katabatic winds can be detected as warm signatures in the surface temperature over the slopes of the Antarctic ice sheets. For appropriate synoptic forcing and/or topographic channeling, katabatic surges occur, which result in warm signatures also over adjacent ice shelves. Mod...
Published in: | Remote Sensing |
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Main Authors: | , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2019
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Subjects: | |
Online Access: | https://doi.org/10.3390/rs11131539 |