ABS
发表于 2025-3-21 16:10:36
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VICT
发表于 2025-3-21 20:46:26
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闲逛
发表于 2025-3-22 03:31:15
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constellation
发表于 2025-3-22 07:40:56
Baroclinic Structure of a Modified Stommel-Arons Model of the Abyssal Ocean Circulationen in Levitus (1982) when the vertical coefficient of thermal diffusion is 125 × 10...s.. The vertical, meridional and zonal components of velocity show significant change in structure from the Stommel — Arons expressions.
MOAN
发表于 2025-3-22 09:29:17
Open Boundary Conditions: Fact and Fiction to avoid possible problems at the lateral boundaries of a limited domain. Moreover, in a fluid such as the atmosphere there is no distinct upper boundary, and most numerical representations of the atmosphere’s vertical structure terminate at some arbitrary level.
Fretful
发表于 2025-3-22 15:05:02
Boundary Filter Initialization of the Hirlam Modelvailable. Such filters have obvious relevance to the problem of initialization for Numerical Weather Prediction. We also discuss some fundamental difficulties encountered when filtering time-limited functions.
Demulcent
发表于 2025-3-22 17:02:44
A Dynamical Stabilizer in the Climate System: A Mechanism Suggested by a Simple Model and Supported re known to exist which could, in principle, drive the climate system far from its observed mean state even in the absence of any external forcings. Extreme scenarios that have been envisaged are a completely ice-covered earth on the one hand and a runaway greenhouse such as appears to have occurred on Venus on the other.
Melatonin
发表于 2025-3-22 23:48:41
Asymptotic Models and Application to Vortex Dynamicsicyclones travel westward faster than cyclones. In FG, vortices of both signs show initially a secondary meridional northward drift which we detail. However this last feature is not present in RSW numerical simulations. Vortices behave like quasi-geostrophic (QG) vortices i.e, showing an initial meridional drift that depends on vortex sign.
肥料
发表于 2025-3-23 02:57:45
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过渡时期
发表于 2025-3-23 05:51:21
An Air-Ocean Coupled Nowcast/Forecast System for the East Asian Marginal Sease Gulf of Tonkin to the YES; a deep, elliptical shaped SCS and JES basins, and numerous reef islands and underwater plateaus scattered throughout (Fig. 1a). The shelf that extends from the Gulf of Tonkin to the YES is consistently near 70 m deep, and averages 150 km in width.