Macroturbulent Equilibration in a Thermally Forced Primitive Equation System
A major question for climate studies is to quantify the role of turbulent eddy fluxes in maintaining the observed ocean–atmosphere state. It has been argued that eddy fluxes keep the midlatitude atmosphere in a state that is marginally critical to baroclinic instability, which provides a powerful co...
| المؤلفون الرئيسيون: | , |
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| مؤلفون آخرون: | |
| التنسيق: | مقال |
| اللغة: | en_US |
| منشور في: |
American Meteorological Society
2012
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| الوصول للمادة أونلاين: | http://hdl.handle.net/1721.1/72983 https://orcid.org/0000-0002-3736-1956 |