Advective temperature change in the 1,000‐700 mb and 700‐500 mb layers
作者:
J. M. Craddock,
期刊:
Quarterly Journal of the Royal Meteorological Society
(WILEY Available online 1951)
卷期:
Volume 77,
issue 331
页码: 51-60
ISSN:0035-9009
年代: 1951
DOI:10.1002/qj.49707733106
出版商: John Wiley&Sons, Ltd
数据来源: WILEY
摘要:
AbstractIt is shown, on the basis of about 700 measurements made at a particular station during six months, that the thermal change in the troposphere due to advection alone is largely offset by the other processes at work, so that the resultant change is a residual having a correlation of about 0.6 with the advective component.The shear hodograph of an upper wind sounding is shown to afford little useful information on the resultant thickness tendency.
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