The Role of Sea Breeze in the Coastal Stratocumulus Dissipation Transition in Antofagasta and San Diego
Coastal Stratocumulus clouds have a diurnal cycle influenced by solar heating and sea-breeze dynamics. These clouds typically thin after sunrise, and some of them fragment and then dissipate, a transition that has proven difficult to predict. In this work, we study the role of sea breeze in the diss...
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| Autori principali: | , , , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
MDPI AG
2025-04-01
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| Serie: | Atmosphere |
| Soggetti: | |
| Accesso online: | https://www.mdpi.com/2073-4433/16/4/437 |
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