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1. Identity statement
Reference TypeConference Paper (Conference Proceedings)
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositorycptec.inpe.br/adm_conf/2005/10.28.15.26
Last Update2006:04.16.18.05.02 (UTC) administrator
Metadata Repositorycptec.inpe.br/adm_conf/2005/10.28.15.26.57
Metadata Last Update2018:06.05.03.42.49 (UTC) administrator
Citation KeyCarrascoBrom:2006:InBeKa
TitleInterannual behaviour of the katabatic wind events across the Ross Ice Shelf
FormatCD-ROM, On-line.
Year2006
Access Date2024, Dec. 27
Secondary TypePRE CI
Number of Files1
Size626 KiB
2. Context
Author1 Carrasco, Jorge
2 Bromwich, David H.
Affiliation1 Dirección Meteorológica de Chile, Casilla 717 Santiago - Chile (Carrasco)
2 Centro de Estudios Científicos, Av. Prat 514, Valdivia - Chile (Carrasco)
3 Polar Meteorology Group, Byrd Polar Research Center, and Atmospheric Science Program, Department of Geography, The Ohio State University, Columbus, Ohio
Author e-Mail Address1 jorge.carrasco@meteochile.cl
2 bromwich@polarmet1.mps.ohio-state.edu
EditorVera, Carolina
Nobre, Carlos
e-Mail Addressjorge.carrasco@meteochile.cl
Conference NameInternational Conference on Southern Hemisphere Meteorology and Oceanography, 8 (ICSHMO).
Conference LocationFoz do Iguaçu
Date24-28 Apr. 2006
PublisherAmerican Meteorological Society (AMS)
Publisher City45 Beacon Hill Road, Boston, MA, USA
Pages183-188
Book TitleProceedings
Tertiary TypeOral
OrganizationAmerican Meteorological Society (AMS)
History (UTC)2005-10-28 15:26:57 :: jorge.carrasco@meteochile.cl -> adm_conf ::
2005-12-15 16:31:21 :: adm_conf -> jorge.carrasco@meteochile.cl ::
2006-03-08 17:57:01 :: jorge.carrasco@meteochile.cl -> administrator ::
2006-04-18 21:01:02 :: administrator -> lise@dpi.inpe.br ::
2010-12-28 12:36:28 :: lise@dpi.inpe.br -> administrator ::
2010-12-29 15:56:25 :: administrator -> lise@dpi.inpe.br :: 2006
2010-12-29 16:05:49 :: lise@dpi.inpe.br -> administrator :: 2006
2010-12-29 18:52:14 :: administrator -> banon :: 2006
2011-01-02 17:14:49 :: banon -> administrator :: 2006
2018-06-05 03:42:49 :: administrator -> :: 2006
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
KeywordsKatabatic winds
Ross Ice Shelf
Antarctic Oscillation
AbstractCold katabatic winds intermittently propagate northwestward from the southernmost region of the Ross Ice Shelf (RIS) toward the Ross Sea, crossing a distance of about 1000 km. Previous pilot studies for April-August 1988, indicate that when these katabatic surge events (KSE) take place the automatic weather stations (AWS) deployed in the southern part of the RIS, in particular the AWS Latteau, reveal an increase in the near surface air temperature, an increase in the pressure gradient normal to the Transantarctic Mountains, an increase wind speed and a more southeasterly wind direction. These findings were applied (meanly the air temperature) to the 1986 - 2004 period for studying the interannual behavior of the katabatic wind events that take place during the winter months April to August. A KSE was defined to occur when the daily average surface-air temperatures recorded by the AWS located in the southern RIS sector were continuously warmer than the respective seasonal mean for at least two days. The winter-annually average of total KSE days is 52 days with a minimum of 41 (in 1992) and a maximum of 62 (in 1994) warmer days associated with KSE. Twelve episodes is the winter annual average of KSE, with a minimum of 9 (in 1999) and maximum 16 events (in 1996). An overall decrease in the number of KSE (and warmer days) is reveal by the linear trend applied to the 1986-2004 period. While an increase of non-KSE (colder days) is revealed by the linear trend. The large-scale compose analysis for the peak of KSE shows an intensified low-pressure center located just to the northwest of Marie Byrd Land along with a mid tropospheric (500 hPa) cyclone center in Ross Sea. A mid-tropospheric cold trough off the RIS reveals that the warm KSE near the surface is associated with cold air mass moving northward from the interior of the Antarctic continent. A preliminary analysis reveals a correlation of 0.63 between the KSE and the ice concentration just offshore of the RIS. Anomalies field for peak-KSE shows a wave number 3 while the anomalies for the peak of non-KSE showed similar pattern of the Antarctic Oscillation (AO), i.e., a negative anomaly region over the continent and positive region centered around 40 -50 ºS latitude belt. Furthermore, a correlation of 0.58 is found between the KSE and the AO index, averaged over the April-August period of the previous year..
AreaMET
TypeClimate and Cryosphere of the Antarctic region
doc Directory Contentaccess
source Directory Content
KSE_8thSHfinala.doc 08/03/2006 14:57 1.4 MiB
agreement Directory Contentthere are no files
4. Conditions of access and use
data URLhttp://urlib.net/ibi/cptec.inpe.br/adm_conf/2005/10.28.15.26
zipped data URLhttp://urlib.net/zip/cptec.inpe.br/adm_conf/2005/10.28.15.26
Languageen
Target File183-188.pdf
User Groupjorge.carrasco@meteochile.cl
administrator
Visibilityshown
5. Allied materials
Host Collectioncptec.inpe.br/nobre/2005/06.02.21.14
cptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
Mark1
Empty Fieldsarchivingpolicy archivist callnumber contenttype copyholder copyright creatorhistory descriptionlevel dissemination documentstage doi edition group identifier isbn issn label lineage mirrorrepository nextedition nexthigherunit notes numberofvolumes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup readpermission resumeid rightsholder schedulinginformation secondarydate secondarykey secondarymark serieseditor session shorttitle sponsor subject tertiarymark url versiontype volume


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