Titlebook: Air-Ice-Ocean Interaction; Turbulent Ocean Boun Miles McPhee Book 2008 Springer-Verlag New York 2008 Ocean.geophysics.geophysics of sea ice

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https://doi.org/10.1007/978-3-662-67084-2binger of climate change. Central to this impact is a thin layer of sea ice that is predominantly seasonal, and at maximum extent (at the end of austral winter) covers roughly 8% of the world ocean area. Sea ice affects climate in several important ways. It effectively insulates the ocean from the c

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遺忘

defibrillator

neoplasm

星球的光亮度

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https://doi.org/10.1007/978-3-8349-8383-1sely on techniques I learned while collaborating with George Mellor when we were both occupying visiting research chairs at the Naval Postgraduate School in Monterey, California. They were first used to model the IOBL with the Mellor-Yamada “l(fā)evel 2.” second-moment closure (Mellor and Yamada 1982; M

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Forum Produkt- und Produktionsmanagementin Chapter 7. The intent is to elucidate certain features of the response of the upper ocean to variations in forcing that require consideration of the time dependence of the physical conservation equations..First, we show that an interesting series of upper ocean measurements at the SHEBA site near

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Vom Bergbau und Hüttenwesen bei den Altenies, along with their Reynolds fluxes including values at the immediate boundary. For the atmospheric surface layer, extensive research has been devoted to methods relating relatively simple measurements to fluxes. Central to this approach is characterizing surface roughness for momentum and scalar

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