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: Ocean Modeling and Parameterization; Eric P. Chassignet,Jacques Verron Book 1998 Springer Science+Business Media Dordrecht 1998 Ocean.Pote

[復(fù)制鏈接]
查看: 9689|回復(fù): 57
樓主
發(fā)表于 2025-3-21 19:11:01 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Ocean Modeling and Parameterization
編輯Eric P. Chassignet,Jacques Verron
視頻videohttp://file.papertrans.cn/701/700497/700497.mp4
叢書名稱Nato Science Series C:
圖書封面Titlebook: Ocean Modeling and Parameterization;  Eric P. Chassignet,Jacques Verron Book 1998 Springer Science+Business Media Dordrecht 1998 Ocean.Pote
描述The realism of large scale numerical ocean models has improved dra- matically in recent years, in part because modern computers permit a more faithful 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 remaining in ocean modeling are associated with parameterizing the effects of these high-frequency, small-space scale processes. Accurate parameterizations are especially needed in long term integrations of coarse resolution ocean models that are designed to understand the ocean vari- ability within the climate system on seasonal to decadal time scales. Traditionally, parameterizations of subgrid-scale, high-frequency mo- tions in ocean modeling have 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
出版日期Book 1998
關(guān)鍵詞Ocean; Potential; Sea ice; computer; convection; dynamics; mixing; turbulent flow
版次1
doihttps://doi.org/10.1007/978-94-011-5096-5
isbn_softcover978-0-7923-5229-7
isbn_ebook978-94-011-5096-5Series ISSN 1389-2185
issn_series 1389-2185
copyrightSpringer Science+Business Media Dordrecht 1998
The information of publication is updating

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(xué)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(xué)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(xué)科排名




書目名稱Ocean Modeling and Parameterization年度引用




書目名稱Ocean Modeling and Parameterization年度引用學(xué)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(xué)科排名




單選投票, 共有 0 人參與投票
 

0票 0%

Perfect with Aesthetics

 

0票 0%

Better Implies Difficulty

 

0票 0%

Good and Satisfactory

 

0票 0%

Adverse Performance

 

0票 0%

Disdainful Garbage

您所在的用戶組沒有投票權(quán)限
沙發(fā)
發(fā)表于 2025-3-21 23:42:47 | 只看該作者
板凳
發(fā)表于 2025-3-22 00:47:41 | 只看該作者
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
地板
發(fā)表于 2025-3-22 06:20:20 | 只看該作者
5#
發(fā)表于 2025-3-22 08:48:14 | 只看該作者
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
6#
發(fā)表于 2025-3-22 14:33:45 | 只看該作者
7#
發(fā)表于 2025-3-22 18:34:44 | 只看該作者
8#
發(fā)表于 2025-3-22 22:17:11 | 只看該作者
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
9#
發(fā)表于 2025-3-23 02:46:44 | 只看該作者
10#
發(fā)表于 2025-3-23 09:34:21 | 只看該作者
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
 關(guān)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(wù)流程 影響因子官網(wǎng) 吾愛論文網(wǎng) 大講堂 北京大學(xué) Oxford Uni. Harvard Uni.
發(fā)展歷史沿革 期刊點(diǎn)評(píng) 投稿經(jīng)驗(yàn)總結(jié) SCIENCEGARD IMPACTFACTOR 派博系數(shù) 清華大學(xué) Yale Uni. Stanford Uni.
QQ|Archiver|手機(jī)版|小黑屋| 派博傳思國(guó)際 ( 京公網(wǎng)安備110108008328) GMT+8, 2025-10-7 11:04
Copyright © 2001-2015 派博傳思   京公網(wǎng)安備110108008328 版權(quán)所有 All rights reserved
快速回復(fù) 返回頂部 返回列表
重庆市| 泰和县| 勃利县| 远安县| 晋城| 壶关县| 东乡| 南涧| 海林市| 汽车| 清涧县| 新源县| 新宁县| 武川县| 英山县| 广宗县| 东海县| 都江堰市| 仪征市| 越西县| 德格县| 沙雅县| 封开县| 紫云| 邯郸县| 陈巴尔虎旗| 五寨县| 朝阳县| 汕尾市| 黑水县| 新宾| 海原县| 海宁市| 太湖县| 鱼台县| 且末县| 陈巴尔虎旗| 五指山市| 宁明县| 庆城县| 保山市|