.png){kind=icon}
返回
Horizontal convection
.png){kind=icon}
PRE
AI
DOI：10.1146/annurev.fluid.40.111406.102148.png)
.png){kind=icon}
原文求助.png){kind=icon}
分享.png){kind=icon}
收藏
摘要
En 中文
Differential heating along one horizontal boundary of a fluid-filled volume establishes an overturning circulation (horizontal convection) in the volume. The governing dynamics in this type of convection are fundamentally different from those in other more commonly studied forms of convection in which the thermal forcing is applied at more than one level. The study of horizontal convection has been motivated largely by the need to understand the role of surface buoyancy forcing of the global oceans, and with this in mind we review a number of extensions to idealized convective flow in a simple box.
Keyword:
differentially heated box
horizontal density gradient
buoyant plume
steady filling box
meridional overturning circulation
AI总结
对已上传原文的论文进行重点信息的提取，主要内容包括：简要概述、研究摘要、背景介绍、关键亮点、图文解析、展望与总结。
期刊
IF:
30.2
论文数:
611
被引数:
1.9W
机构
引用论文
A simple convective model of the global overturning circulation, including effects of entrainment into sinking regions.png)
OCEAN MODELLING
OCEAN MODELLINGIF2.9
PREAI
分享收藏
分享收藏
查看更多内容