Planetary Wave Breaking and Tropospheric Forcing as Seen in the Stratospheric Sudden Warming of 2006

The major stratospheric sudden warming (SSW) of January 2006 is examined using meteorological fields from Goddard Earth Observing System version 4 (GEOS-4) analyses and forecast fields from the Navy Operational Global Atmospheric Prediction System-Advanced Level Physics, High Altitude (NOGAPS-ALPHA)...

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Bibliographic Details
Main Authors: Coy, Lawrence, Eckermann, Stephen, Hoppel, Karl
Other Authors: NAVAL RESEARCH LAB WASHINGTON DC
Format: Text
Language:English
Published: 2009
Subjects:
Atmospheric Physics
*ATMOSPHERE MODELS
TROPICAL REGIONS
STRATOSPHERE
WAVES
REPRINTS
TROPOSPHERE
SSW(STRATOSPHERIC SUDDEN WARMING)
WAVE BREAKING
PV(POTENTIAL VORTICITY)
GEOS-4(GODDARD EARTH OBSERVING SYSTEM VERSION 4)
North Atlantic
Online Access:http://www.dtic.mil/docs/citations/ADA520947
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA520947
Description
Summary:The major stratospheric sudden warming (SSW) of January 2006 is examined using meteorological fields from Goddard Earth Observing System version 4 (GEOS-4) analyses and forecast fields from the Navy Operational Global Atmospheric Prediction System-Advanced Level Physics, High Altitude (NOGAPS-ALPHA). The study focuses on the upper tropospheric forcing that led to the major SSW and the vertical structure of the subtropic wave breaking near 10 hPa that moved low tropical values of potential vorticity (PV) to the pole. Results show that an eastward-propagating upper tropospheric ridge over the North Atlantic with its associated cold temperature perturbations (as manifested by high 360-K potential temperature surface perturbations) and large positive local values of meridional heat flux directly forced a change in the stratospheric polar vortex, leading to the stratospheric subtropical wave breaking and warming. Results also show that the anticyclonic development, initiated by the subtropical wave breaking and associated with the poleward advection of the low PV values, occurred over a limited altitude range of approximately 6-10 km. The authors also show that the poleward advection of this localized low-PV anomaly was associated with changes in the Eliassen-Palm (EP) flux from equatorward to poleward, suggesting an important role for Rossby wave reflection in the SSW of January 2006. Similar upper tropospheric forcing and subtropical wave breaking were found to occur prior to the major SSW of January 2003. Published in Journal of the Atmospheric Sciences, v66 p495-507, Feb 2009. Supported in part by NASA.

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