完整
发表于 2025-3-28 16:30:47
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archenemy
发表于 2025-3-28 19:57:48
Forced Wavesct and can be created by other waves. We have discussed a general treatment in Section 9.6, using a Lagrangian framework. We expand the treatment to a situation where a random ensemble of waves is an adequate representation for the wave field.
brassy
发表于 2025-3-29 00:00:34
Geostrophic Turbulencection 12.2 is devoted to the more realistic inhomogeneous situation of the real ocean. In Section 12.3 we discuss alternative averaging frameworks to differentiate between advective and diffusive effects of turbulent mixing.
不规则
发表于 2025-3-29 03:42:42
Small-Scale Turbulenceiscussed in Section 11.1, while basic concepts of turbulent mixing are described in Section 11.2. The application to the real, i. e. inhomogeneous, ocean in the presence of density stratification and large gravity force and the development of basic turbulence closure schemes can be found in Section 11.3.
strdulate
发表于 2025-3-29 11:15:07
The Wind-Driven Circulationstigated using the model BARBI. This model represents the interaction of barotropic and baroclinic fields in a minimal way. The spin-up of the wind-driven circulation by wave processes was presented in Section 8.2.6.
Constant
发表于 2025-3-29 14:37:59
Physics of Heat Exchange with the Environment,t temperature difference (. .C.). In the case of evaporation on the skin, the water vapour pressure difference (.) between the body surface and the ambient air substitutes for the temperature difference.
Apogee
发表于 2025-3-29 17:37:36
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CHURL
发表于 2025-3-29 22:01:13
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类人猿
发表于 2025-3-30 01:45:21
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分散
发表于 2025-3-30 05:22:57
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