找回密碼
 To register

QQ登錄

只需一步,快速開始

掃一掃,訪問微社區(qū)

打印 上一主題 下一主題

Titlebook: Large-Scale Transport Processes in Oceans and Atmosphere; J. Willebrand,D. L. T. Anderson Book 1986 Springer Science+Business Media Dordre

[復制鏈接]
樓主: MOURN
11#
發(fā)表于 2025-3-23 13:05:30 | 只看該作者
Thermohaline Effects in the Ocean Circulation and Related Simple Models,mportant role for the development of physical oceanography in Scandinavia. Helland-Hansen, Nansen, Ekman and their collaborators in the “Bergen School” developed the instruments needed to measure these and other oceanographic parameters of interest with the required accuracy. They also developed the
12#
發(fā)表于 2025-3-23 15:06:34 | 只看該作者
13#
發(fā)表于 2025-3-23 21:30:12 | 只看該作者
,Wind Driven Ocean Circulation Theory — Steady Free Flow,he motion. Particular emphasis is placed on steady free flows in which q is constant along a streamline of the flow ψ. The importance of weak forcing and dissipation in removing the indeterminacy of inviscid theory is stressed. Ways of extending the theory to baroclinic flow are suggested.
14#
發(fā)表于 2025-3-24 01:57:59 | 只看該作者
Coupled Ocean-Atmosphere Models of El Nino and the Southern Oscillation,an equation for the temperature of the layer, T. The model atmosphere is a linear, single-baroclinic mode system driven by convection, Q. The wind stress used to drive the model ocean is proportional to the wind velocity produced by the model atmosphere, while Q over the ocean is a function only of
15#
發(fā)表于 2025-3-24 02:29:45 | 只看該作者
16#
發(fā)表于 2025-3-24 08:49:22 | 只看該作者
17#
發(fā)表于 2025-3-24 13:51:41 | 只看該作者
Some Aspects of Turbulent Diffusion,iffusion. The quantities transported by the flow can be passive or active. If one is interested in ocean or atmosphere dynamics, these quantities are for instance the temperature, momentum, potential vorticity, Lagrangian tracers, error (this entity will be defined later), and others.
18#
發(fā)表于 2025-3-24 18:48:13 | 只看該作者
Turbulent Diffusion in Large-Scale Flows,n the ocean, and the way to parameterize them in numerical models. By turbulent diffusion, we mean the mean effect of small scales on the larger scales: these “small” scales are barotropic and baroclinic transient eddies which we may not necessarily want to resolve in our numerical simulations — esp
19#
發(fā)表于 2025-3-24 20:15:01 | 只看該作者
sinnlichen ?hnlichkeit“ von Figur und Figuriertem, und wer an den Elementen der Schrift und an Bildern als Gefügen nicht deutend wie an Emblemen sich versuchte, darf nicht hoffen, der Dinge selbst als Figurationen gewahr zu werde. Das sich selbst Limitieren und Substantiieren des Wirklichen, das Au?
20#
發(fā)表于 2025-3-25 01:09:32 | 只看該作者
 關于派博傳思  派博傳思旗下網(wǎng)站  友情鏈接
派博傳思介紹 公司地理位置 論文服務流程 影響因子官網(wǎng) 吾愛論文網(wǎng) 大講堂 北京大學 Oxford Uni. Harvard Uni.
發(fā)展歷史沿革 期刊點評 投稿經(jīng)驗總結 SCIENCEGARD IMPACTFACTOR 派博系數(shù) 清華大學 Yale Uni. Stanford Uni.
QQ|Archiver|手機版|小黑屋| 派博傳思國際 ( 京公網(wǎng)安備110108008328) GMT+8, 2025-10-11 02:08
Copyright © 2001-2015 派博傳思   京公網(wǎng)安備110108008328 版權所有 All rights reserved
快速回復 返回頂部 返回列表
自贡市| 汶上县| 班玛县| 丽江市| 临邑县| 礼泉县| 咸宁市| 彝良县| 聊城市| 漾濞| 南川市| 隆子县| 东乡县| 铁力市| 阿拉善右旗| 潮州市| 布拖县| 仙游县| 日喀则市| 莱州市| 广河县| 闸北区| 平山县| 黄浦区| 内江市| 通榆县| 钟山县| 贡嘎县| 出国| 东山县| 金沙县| 都匀市| 呼图壁县| 台东市| 日喀则市| 德庆县| 湖州市| 瓦房店市| 新巴尔虎右旗| 东平县| 图木舒克市|