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...
| المؤلفون الرئيسيون: | , |
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| التنسيق: | مقال |
| اللغة: | English |
| منشور في: |
Stockholm University Press
2014-09-01
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| سلاسل: | Tellus: Series A, Dynamic Meteorology and Oceanography |
| الموضوعات: | |
| الوصول للمادة أونلاين: | http://www.tellusa.net/index.php/tellusa/article/download/24041/pdf_1 |