Earth's Sea Ice Radiative Effect From 1980 to 2023
Abstract Sea ice cools Earth by reducing its absorbed solar energy. We combine radiative transfer modeling with satellite‐derived surface albedo, sea ice, and cloud distributions to quantify the top‐of‐atmosphere sea ice radiative effect (SIRE). Averaged over 1980–2023, Arctic and Antarctic SIREs ra...
| Hoofdauteurs: | , , |
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| Formaat: | Artikel |
| Taal: | English |
| Gepubliceerd in: |
Wiley
2024-07-01
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| Reeks: | Geophysical Research Letters |
| Online toegang: | https://doi.org/10.1029/2024GL109608 |