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contributor authorSteenrod, Stephen D.
contributor authorRood, Richard B.
contributor authorLamich, David J.
contributor authorRosenfield, Joan E.
contributor authorGovindaraju, Ravi C.
date accessioned2017-06-09T16:08:38Z
date available2017-06-09T16:08:38Z
date copyright1992/01/01
date issued1992
identifier issn0027-0644
identifier otherams-61907.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4202740
description abstractUsing a stratospheric-tropospheric data assimilation system, referred to as STRATAN, a minor sudden stratospheric warming that occurred in January 1989 is investigated. The event had a maximum influence on the stratospheric circulation near 2 hPa. The zonal mean circulation reversed briefly in the polar region as the temperature increased 34 K in 3 days. The cause of the warming is shown to be the rapid development and subsequent movement of a warm anomaly, which initially developed in the midlatitudes. The development of the warm anomaly is caused by adiabatic descent, and the dissipation by radiative cooling. A brief comparison with the NMC analysis and temperature sounding data is also presented.
publisherAmerican Meteorological Society
titleThe Minor Stratospheric Warming of January 1989: Results from STRATAN, a Stratospheric-Tropospheric Data Assimilation System
typeJournal Paper
journal volume120
journal issue1
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1992)120<0221:TMSWOJ>2.0.CO;2
journal fristpage221
journal lastpage229
treeMonthly Weather Review:;1992:;volume( 120 ):;issue: 001
contenttypeFulltext


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