Modelling the impact of Baltic Sea upwelling on the atmospheric boundary layer

Coastal upwelling, with a strong sea-surface temperature (SST) signal, is extremely common in the Baltic Sea during the summer months. Although the spatial scale of upwelling is small, its high frequency of occurrence in the semi-enclosed basin may allow the SST signature to have significant feedbac...

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Những tác giả chính: David Sproson, Erik Sahlée
Định dạng: Bài viết
Ngôn ngữ:English
Được phát hành: Stockholm University Press 2014-09-01
Loạt:Tellus: Series A, Dynamic Meteorology and Oceanography
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Truy cập trực tuyến:http://www.tellusa.net/index.php/tellusa/article/download/24041/pdf_1