Steady Convective Motion in a Horizontal Layer of Fluid Heated Uniformly from Above and Cooled Non-uniformly from Below-Reference-Cited by-同舟云学术

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Steady Convective Motion in a Horizontal Layer of Fluid Heated Uniformly from Above and Cooled Non-uniformly from Below

Published:1957-01 Issue:3 Volume:9 Page:401-407
ISSN:0040-2826
Container-title:Tellus
language:en
Short-container-title:Tellus

Author:

Stommel Henry¹,Veronis George¹

Affiliation:

1. Woods Hole Oceanographic Institution

Publisher

Informa UK Limited

Subject

General Medicine

Link

https://www.tandfonline.com/doi/pdf/10.3402/tellusa.v9i3.9100

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3. An analytical model of an urban heat island circulation in calm conditions;Environmental Fluid Mechanics;2018-08-21

4. On one mechanism of gravity field inhomogeneities influence on atmosphere dynamics;Technical Physics;2017-09

5. Dynamic Properties of Diurnal and Annual Horizontal Convections in the Japanese Islands;SOLA;2011

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