Boundary Layer Convergence Induced by Strong Winds across a Midlatitude SST Front*
نویسندگان
چکیده
منابع مشابه
Reductions in midlatitude upwelling-favorable winds implied by weaker large-scale Pliocene SST gradients
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The early-to-mid Pliocene (3–5.3 Ma) is the most recent geologic period of significant global warmth. Proxy records of Pliocene sea surface temperature (SST) indicate significant and still unexplained warm anomalies of 3∘C–9∘C in midlatitude eastern boundary currents, where present-day cool temperatures are maintained by wind-driven upwelling. Here we quantify the effect of large-scale Pliocene...
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The main goal of the proposed research is to study theoretically the role of the breaking wind waves and the sea spray, generated by them, under strongly forced situations in the airflow dynamics in particular in energy, momentum, heat and moisture transfers through the sea surface. Through this to increase the knowledge of the air-sea interaction and to apply this knowledge for developing impr...
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ژورنال
عنوان ژورنال: Journal of Climate
سال: 2014
ISSN: 0894-8755,1520-0442
DOI: 10.1175/jcli-d-13-00101.1