Change from aerosol-driven to cloud-feedback-driven trend in short-wave radiative flux over the North Atlantic
<p>Aerosol radiative forcing and cloud–climate feedbacks each have a large effect on climate, mainly through modification of solar short-wave radiative fluxes. Here we determine what causes the long-term trends in the upwelling short-wave (SW) top-of-the-atmosphere (TOA) fluxes (<span class="inline-...
Αποθηκεύτηκε σε:
| Κύριοι συγγραφείς: | , |
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| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
Copernicus Publications
2023-06-01
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| Σειρά: | Atmospheric Chemistry and Physics |
| Διαθέσιμο Online: | https://acp.copernicus.org/articles/23/6743/2023/acp-23-6743-2023.pdf |
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