Aggrief
发表于 2025-3-21 19:11:01
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verdict
发表于 2025-3-21 23:42:47
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不出名
发表于 2025-3-22 00:47:41
Forcing the Ocean,ins…”, and it could continue as: “… and therefore the physical boundaries of the ocean are the bottom of the basins, the coastlines, and the free surface in permanent contact with the atmosphere”. Heat entering the ocean through the bottom of the basins is usually considered as negligible. Estimates
Isolate
发表于 2025-3-22 06:20:20
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absorbed
发表于 2025-3-22 08:48:14
Parameterization of the Fair Weather Ekman Layer,re and compared with fair weather data sets. A steady classical diffusion model is found to give reasonably good simulations with familiar values of diffusivity. However, the solutions show a systematic error in current direction that arises, apparently, from a non-parallel relation between shear an
Amylase
发表于 2025-3-22 14:33:45
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Diskectomy
发表于 2025-3-22 18:34:44
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Panther
发表于 2025-3-22 22:17:11
Turbulent Mixing in the Ocean,of order 10.m) are limited chiefly by the size of ocean basins and ultimately of the earth. On the other end of the spectrum, gradients in velocity and water properties exist to sub-meter scales (see below). The total range of spatial scales is thus some nine or more orders of magnitude. The tempera
Amenable
发表于 2025-3-23 02:46:44
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OUTRE
发表于 2025-3-23 09:34:21
Double-Diffusive Convection, of the two orders of magnitude difference between the thermal conductivity of water and the diffusivity of dissolved salts, and the tendency of gradients of temperature and salinity to oppose one another in their effects on density. This leads to a number of counter-intuitive effects, such as up-gr