標題: Titlebook: Ocean Modeling and Parameterization; Eric P. Chassignet,Jacques Verron Book 1998 Springer Science+Business Media Dordrecht 1998 Ocean.Pote [打印本頁] 作者: Aggrief 時間: 2025-3-21 19:11
書目名稱Ocean Modeling and Parameterization影響因子(影響力)
書目名稱Ocean Modeling and Parameterization影響因子(影響力)學科排名
書目名稱Ocean Modeling and Parameterization網(wǎng)絡(luò)公開度
書目名稱Ocean Modeling and Parameterization網(wǎng)絡(luò)公開度學科排名
書目名稱Ocean Modeling and Parameterization被引頻次
書目名稱Ocean Modeling and Parameterization被引頻次學科排名
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書目名稱Ocean Modeling and Parameterization年度引用學科排名
書目名稱Ocean Modeling and Parameterization讀者反饋
書目名稱Ocean Modeling and Parameterization讀者反饋學科排名
作者: verdict 時間: 2025-3-21 23:42 作者: 不出名 時間: 2025-3-22 00:47
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作者: Isolate 時間: 2025-3-22 06:20 作者: absorbed 時間: 2025-3-22 08:48
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作者: Amylase 時間: 2025-3-22 14:33 作者: Diskectomy 時間: 2025-3-22 18:34 作者: Panther 時間: 2025-3-22 22:17
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作者: Amenable 時間: 2025-3-23 02:46 作者: OUTRE 時間: 2025-3-23 09:34
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作者: 領(lǐng)袖氣質(zhì) 時間: 2025-3-23 09:59
Interleaving at the Equator,ent studies have shown that for the ENSO phenomenom the predictability of coupled models is very dependent on the initial state of the ocean model (. Latif and Graham, [.]). What dictates the state of the ocean, its density and current structure, is still a matter for debate. Neelin . [.] suggest th作者: generic 時間: 2025-3-23 16:23
Eddy Parameterisation in Large Scale Flow,en the need for simulations of centuries to examine climate issues, and the enormous computer resources necessary to undertake such integrations while retaining at least some degree of eddy activity in the model. For the foreseeable future, climate models will have to continue to include parameteris作者: 教唆 時間: 2025-3-23 21:41 作者: 誓言 時間: 2025-3-23 23:55
Statistical Mechanics of Potential Vorticity for Parameterizing Mesoscale Eddies,ded diffusion current) in parameterizing the diffusion of a conserved quantity. In the case of potential vorticity, complete mixing is forbidden by energy conservation, and the MEP leads to a subgrid-scale parameterization with a diffusion term, but also with a drift term. The end result of the free作者: Priapism 時間: 2025-3-24 04:56
Topographic Stress: Importance and Parameterization,ced by the break up of the continents. This nonlinear nature of ocean dynamics generates a wide variety of interesting physical phenomena mainly related to the existence of strong dynamical links among physical processes occurring at different space and time scales. These links range from space scal作者: 不能平靜 時間: 2025-3-24 10:26 作者: CRAMP 時間: 2025-3-24 11:09 作者: 粉筆 時間: 2025-3-24 15:15
,On the Large-Scale Modeling of Sea Ice and Sea Ice—Ocean Interactions,nd slow current rivers, sea ice forms not only at the surface but also underwater. This is due to the fact that, for typical ocean salinities, the seawater density increases monotonically with decreasing temperature, and therefore surface cooling generates continued convective overturning until the 作者: 拱形大橋 時間: 2025-3-24 21:56 作者: Antagonist 時間: 2025-3-25 00:37
Forcing the Ocean,onto the abyssal plain. The entire budget for the world ocean is roughly 10.., which is thought to be carried by the hydrothermal part; the conductive part is a similar order of magnitude. For comparison, the annual mean solar heat flux entering the ocean from the sea surface is above 150 .. on aver作者: 沙草紙 時間: 2025-3-25 06:55 作者: 草率男 時間: 2025-3-25 09:28 作者: 享樂主義者 時間: 2025-3-25 13:36
Parameter Estimation in Dynamical Models,s in which data assimilation methods have been used to improve estimates of poorly known model parameters or even the model bias will be briefly reviewed. that [.] . the first-guess values of the parameters with the . in each iteration of the parameters. These should of course be kept constant. Clea作者: Carcinogenesis 時間: 2025-3-25 16:01 作者: 機構(gòu) 時間: 2025-3-25 23:29
Book 1998have been based on simple formulations, such as the Reynolds decomposition with constant diffusivity values. Until recently, modelers were concerned with first order issues such as a correct represen- tation of the basic features of the ocean circulation. As the numerical simu- lations become better作者: 勉強 時間: 2025-3-26 03:31 作者: BILK 時間: 2025-3-26 08:23 作者: 未完成 時間: 2025-3-26 10:18 作者: employor 時間: 2025-3-26 15:14 作者: 指令 時間: 2025-3-26 17:08 作者: irradicable 時間: 2025-3-27 00:03 作者: Antagonist 時間: 2025-3-27 01:19 作者: STRIA 時間: 2025-3-27 08:32 作者: 暫時別動 時間: 2025-3-27 11:33 作者: 考博 時間: 2025-3-27 15:30
Parameterization of the Fair Weather Ekman Layer,diurnal cycle is likely to be important in fair weather conditions. The process of diurnal cycling can be treated in a layered model to yield a closed solution for Ekman layer currents. This solution has some of the characteristics of a useful parameterization for use in an OGCM, though it covers only a part of the relevant parameter range.作者: 舊石器 時間: 2025-3-27 21:40
Marginal Sea Overflows for Climate Simulations,Compared to an OGCM solution without a marginal sea, but one which still has a vigorous thermohaline circulation, the combined model solution has much better deep water properties and a rather different circulation in the northern basin.作者: 可以任性 時間: 2025-3-27 22:51
Interleaving at the Equator,ameters used in subgrid scale processes. McPhaden [.] notes the importance of improving model physics, through parameterizing small scale mixing processes, to accurately model the equatorial ocean and predict El Ni?o.作者: 公式 時間: 2025-3-28 05:57
Statistical Mechanics of Potential Vorticity for Parameterizing Mesoscale Eddies,e drift term corresponds to the Neptune effect of Holloway (.). Application to a wind-driven barotropic ocean basin is presented, and extensions to baroclinic cases are sketched. A more mechanistic approach, using kinetic models, confirms the existence of the drift term and estimates the diffusivity.作者: 蹣跚 時間: 2025-3-28 08:43
Book 1998 representation of the differential equations by their algebraic analogs. Equally significant, if not more so, has been the improved under- standing of physical processes on space and time scales smaller than those that can be represented in such models. Today, some of the most challeng- ing issues 作者: 滋養(yǎng) 時間: 2025-3-28 14:12
Modeling and Parameterizing the Ocean Planetary Boundary Layer,e OBL. The ocean’s benthic boundary layer and its parameterization are the subjects of Beckmann (1998, this volume). Shallow coastal regions where the OBL and benthic boundary layer interact, and where ocean tidal mixing can be strong are excluded. Also excluded are ocean interior mixing processes, except when they interact with the OBL.作者: 本能 時間: 2025-3-28 17:56 作者: 幸福愉悅感 時間: 2025-3-28 19:44 作者: 高深莫測 時間: 2025-3-29 00:44 作者: figure 時間: 2025-3-29 04:04
Ocean Modeling and Parameterization978-94-011-5096-5Series ISSN 1389-2185 作者: agglomerate 時間: 2025-3-29 09:06 作者: Metamorphosis 時間: 2025-3-29 15:09 作者: negligence 時間: 2025-3-29 19:32 作者: 猛烈責罵 時間: 2025-3-29 23:19
The End of the Hyperinflation and Its Consequences,public as early as March and April of the same year, and with greater intensity, of course, in June and July. Moreover, negotiations with the unionized labour force under the control of the Communist Party produced a settlement on a post-stabilization wage. It was clearly understood that the burdens作者: AV-node 時間: 2025-3-30 02:41 作者: 時間等 時間: 2025-3-30 07:41 作者: 統(tǒng)治人類 時間: 2025-3-30 11:21
Cutaneous Thermoreceptionthe reader to comprehensive works on thermoreceptors (., 1952 a, 1966, 1973; ., 1959) and patterns of behavior of homeotherms under thermal stimulation (., 1952; ., ., and ., 1970; ., 1970, 1971; ., 1971). Thermosensitive structures in the central nervous system are dealt with on p. 567.作者: 歡呼 時間: 2025-3-30 15:13 作者: 欺騙世家 時間: 2025-3-30 17:57
vivo. More importantly, in the last few years, we have witnessed significant efforts and progress in elucidating the mechanisms underlying synthetic vector-mediated DNA delivery. With the continuous effort to meet the need for safe and efficient gene-delivery methods for human gene therapy, it is fo作者: Cosmopolitan 時間: 2025-3-30 23:50 作者: discord 時間: 2025-3-31 00:55
Klaus Northfically, under what conditions can we expect external actors to have an impact on domestic politics? How do external and internal actors interact with one another in processes of externally led political reform?作者: 忘恩負義的人 時間: 2025-3-31 06:52 作者: 沙發(fā) 時間: 2025-3-31 11:45 作者: output 時間: 2025-3-31 16:38
