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contributor authorCoy, Lawrence
contributor authorRood, Richard B.
contributor authorNewman, Paul A.
date accessioned2017-06-09T14:32:25Z
date available2017-06-09T14:32:25Z
date copyright1994/08/01
date issued1994
identifier issn0022-4928
identifier otherams-21247.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157565
description abstractWinds derived from a stratospheric and tropospheric data assimilation system (STRATAN) are compared with balance winds derived from National Meteorological Center/Climate Analysis Center (NMC/CAC) heights. At middle latitudes in the lower stratosphere, the results show that STRATAN winds are comparable to the balance winds. In addition STRATAN winds provide useful horizontal divergence analyses, and hence, vertical velocity fields. More generally, the STRATAN winds are useful in a more extended domain than the balanced winds. In particular, they are useful in the Tropics and the upper stratosphere where the balanced winds fail. The assimilation also captures the quasi-biennial oscillation, but does not do a good job of representing tropical waves.
publisherAmerican Meteorological Society
titleA Comparison of Winds from the STRATAN Data Assimilation System to Balanced Wind Estimates
typeJournal Paper
journal volume51
journal issue15
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1994)051<2309:ACOWFT>2.0.CO;2
journal fristpage2309
journal lastpage2315
treeJournal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 015
contenttypeFulltext


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