The Major Stratospheric Sudden Warming of January 2013: Analyses and Forecasts in the GEOS-5 Data Assimilation System

We examine the major stratosphere sudden warming (SSW) that occurred on 6 January 2013, using output from the NASA Global Modeling and Assimilation Office (GMAO) GEOS-5 (Goddard Earth Observing System) near-real-time data assimilation system (DAS). Results show that the major SSW of January 2013 fal...

Full description

Bibliographic Details
Main Authors: Coy, Lawrence, Pawson, Steven
Format: Other/Unknown Material
Language:unknown
Published: 2014
Subjects:
Online Access:http://hdl.handle.net/2060/20140012679
id ftnasantrs:oai:casi.ntrs.nasa.gov:20140012679
record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:20140012679 2023-05-15T17:34:14+02:00 The Major Stratospheric Sudden Warming of January 2013: Analyses and Forecasts in the GEOS-5 Data Assimilation System Coy, Lawrence Pawson, Steven Unclassified, Unlimited, Publicly available February 16, 2014 application/pdf http://hdl.handle.net/2060/20140012679 unknown Document ID: 20140012679 http://hdl.handle.net/2060/20140012679 Copyright, Distribution as joint owner in the copyright CASI Meteorology and Climatology GSFC-E-DAA-TN12939 2014 ftnasantrs 2019-07-21T06:13:24Z We examine the major stratosphere sudden warming (SSW) that occurred on 6 January 2013, using output from the NASA Global Modeling and Assimilation Office (GMAO) GEOS-5 (Goddard Earth Observing System) near-real-time data assimilation system (DAS). Results show that the major SSW of January 2013 falls into the vortex splitting type of SSW, with the initial planetary wave breaking occurring near 10 hPa. The vertical flux of wave activity at the tropopause responsible for the SSW occurred mainly in the Pacific Hemisphere, including the a pulse associated with the preconditioning of the polar vortex by wave 1 identified on 23 December 2012. While most of the vertical wave activity flux was in the Pacific Hemisphere, a rapidly developing tropospheric weather system over the North Atlantic on 28 December is shown to have produced a strong transient upward wave activity flux into the lower stratosphere coinciding with the peak of the SSW event. In addition, the GEOS-5 5-day forecasts accurately predicted the major SSW of January 2013 as well as the upper tropospheric disturbances responsible for the warming. The overall success of the 5-day forecasts provides motivation to produce regular 10-day forecasts with GEOS-5, to better support studies of stratosphere-troposphere interaction. Other/Unknown Material North Atlantic NASA Technical Reports Server (NTRS) Pacific
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic Meteorology and Climatology
spellingShingle Meteorology and Climatology
Coy, Lawrence
Pawson, Steven
The Major Stratospheric Sudden Warming of January 2013: Analyses and Forecasts in the GEOS-5 Data Assimilation System
topic_facet Meteorology and Climatology
description We examine the major stratosphere sudden warming (SSW) that occurred on 6 January 2013, using output from the NASA Global Modeling and Assimilation Office (GMAO) GEOS-5 (Goddard Earth Observing System) near-real-time data assimilation system (DAS). Results show that the major SSW of January 2013 falls into the vortex splitting type of SSW, with the initial planetary wave breaking occurring near 10 hPa. The vertical flux of wave activity at the tropopause responsible for the SSW occurred mainly in the Pacific Hemisphere, including the a pulse associated with the preconditioning of the polar vortex by wave 1 identified on 23 December 2012. While most of the vertical wave activity flux was in the Pacific Hemisphere, a rapidly developing tropospheric weather system over the North Atlantic on 28 December is shown to have produced a strong transient upward wave activity flux into the lower stratosphere coinciding with the peak of the SSW event. In addition, the GEOS-5 5-day forecasts accurately predicted the major SSW of January 2013 as well as the upper tropospheric disturbances responsible for the warming. The overall success of the 5-day forecasts provides motivation to produce regular 10-day forecasts with GEOS-5, to better support studies of stratosphere-troposphere interaction.
format Other/Unknown Material
author Coy, Lawrence
Pawson, Steven
author_facet Coy, Lawrence
Pawson, Steven
author_sort Coy, Lawrence
title The Major Stratospheric Sudden Warming of January 2013: Analyses and Forecasts in the GEOS-5 Data Assimilation System
title_short The Major Stratospheric Sudden Warming of January 2013: Analyses and Forecasts in the GEOS-5 Data Assimilation System
title_full The Major Stratospheric Sudden Warming of January 2013: Analyses and Forecasts in the GEOS-5 Data Assimilation System
title_fullStr The Major Stratospheric Sudden Warming of January 2013: Analyses and Forecasts in the GEOS-5 Data Assimilation System
title_full_unstemmed The Major Stratospheric Sudden Warming of January 2013: Analyses and Forecasts in the GEOS-5 Data Assimilation System
title_sort major stratospheric sudden warming of january 2013: analyses and forecasts in the geos-5 data assimilation system
publishDate 2014
url http://hdl.handle.net/2060/20140012679
op_coverage Unclassified, Unlimited, Publicly available
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_source CASI
op_relation Document ID: 20140012679
http://hdl.handle.net/2060/20140012679
op_rights Copyright, Distribution as joint owner in the copyright
_version_ 1766132993265500160