The vertical convective heat flux in the atmosphere—a critical essay
作者:
G. D. Robinson,
期刊:
Quarterly Journal of the Royal Meteorological Society
(WILEY Available online 1951)
卷期:
Volume 77,
issue 331
页码: 61-73
ISSN:0035-9009
年代: 1951
DOI:10.1002/qj.49707733107
出版商: John Wiley&Sons, Ltd
数据来源: WILEY
摘要:
AbstractA definition of convective vertical heat flux is proposed which leads directly to the expressionp1w1h1wherep1,w1, andh1are, respectively, simultaneous values of the fluctuating density, vertical velocity relative to the surface, and total heat per unit mass at a point in a constant pressure surface. Neglect (apparently justifiable) of the pressure fluctuations yields the expressioncpp±w1/Rfor the convective flux of sensible heat. The distinction between free and forced convection is made. Recent treatments by Montgomery and by Priestley and Swinbank are examined with particular attention to the importance of free convection. It is submitted that neither Montgomery's neglect of the buoyancy forces nor Priestley and Swinbank's arguments suggesting their universal importance can at present be justified. In particular the latter authors explanation of the normal tropospheric lapse rate is questioned
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