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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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Hlavní autoři: Gabriela Pallauta Pérez, Ricardo C. Muñoz, Patricio Arrué, Mónica Zamora Zapata
Médium: Artigo
Jazyk:Inglês
Vydáno: MDPI AG 2025-04-01
Edice:Atmosphere
Témata:
stratocumulus
sea breeze
cloud fragmentation
cloud dissipation
On-line přístup:https://www.mdpi.com/2073-4433/16/4/437
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