Trends and spatial variation in rain-on-snow events over the Arctic Ocean during the early melt season
Rain-on-snow (ROS) events can accelerate the surface ablation of sea ice, thus greatly influencing the ice–albedo feedback. However, the variability of ROS events over the Arctic Ocean is poorly understood due to limited historical station data in this region. In this study early melt season ROS eve...
Published in: | The Cryosphere |
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Main Authors: | , , , , , , , , , , , |
Format: | Text |
Language: | English |
Published: |
2021
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-15-883-2021 https://tc.copernicus.org/articles/15/883/2021/ |