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File:Thermohaline Circulation using Improved Flow Field.ogv

Thermohaline_Circulation_using_Improved_Flow_Field.ogv ‎（Ogg Theora视频文件，长度2分47秒，640 × 216像素，697 kbps，文件大小：13.86 MB）

摘要

描述
English: The colouring of the world's oceans at the beginning of this animation represents surface water density, with dark regions being most dense and light regions being least dense (see the animation Sea Surface Temperature, Salinity and Density). Heights and (especially) depths of the oceans are greatly exaggerated (20x on land, 100x in oceans) to better illustrate the differences between the surface flows and deep water flows. Note that this animation presents the flows as described in current models and theories of the thermohaline circulation, not actual observed data. (The thermohaline circulation is a very slow moving current that can be difficult to distinguish from general ocean circulation, making it difficult to measure or simulate.)
日期
来源 Goddard Multimedia
作者 NASA/Goddard Space Flight Center

许可协议

Public domain 本文件完全由NASA创作，在美国属于公有领域。根据NASA的版权方针，NASA的材料除非另有声明否则不受版权保护。（参见Template:PD-USGov/zh、NASA版权方针页面或JPL图片使用方针。）
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当前2011年12月7日 (三) 17:462分47秒, 640 × 216（13.86 MB）Originalwana{{Information |Description ={{en|1=The colour on the world's ocean's at the beginning of this animation represents surface water density, with dark regions being most dense and light regions being least dense (see the animation Sea Surface Temperature,

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