Snow accumulation variability in Wilkes land, East Antarctica, and the relationship to atmospheric ridging in the 130°-170°E region since 1930
Identifieur interne : 004E06 ( PascalFrancis/Checkpoint ); précédent : 004E05; suivant : 004E07Snow accumulation variability in Wilkes land, East Antarctica, and the relationship to atmospheric ridging in the 130°-170°E region since 1930
Auteurs : I. Goodwin [Australie] ; M. De Angelis [France] ; M. Pook [Australie] ; N. W. Young [Australie]Source :
- Journal of geophysical research [ 0148-0227 ] ; 2003.
Descripteurs français
- Pascal (Inist)
- Accumulation neige, Ionosphère région E, Variation annuelle, Carotte, Circulation atmosphérique, Série temporelle, Masse air, Inlandsis, Fluctuation, Intensification, Variation interannuelle, Taux accumulation, Trajectoire, Cyclolyse, Onde longue, Neige, Hiver, Niveau mer, Gradient pression, Hauteur géopotentielle, Antarctique, Nouvelle Zélande, Australie, Vent zonal, Vent surface, Troposphère, Névé, Mode annulaire.
- Wicri :
- geographic : Australie.
English descriptors
- KwdEn :
- Accumulation rate, Air mass, Annular mode, Antarctica, Australia, Cyclolysis, Geopotential height, Intensification, Interannual variation, Ionospheric E region, Long wave, New Zealand, Pressure gradient, Snow accumulation, Surface wind, Time series, Winter, Zonal wind, annual variations, atmospheric circulation, drill cores, firn, fluctuations, ice sheets, sea level, snow, trajectory, troposphere.
Abstract
[i] Wilkes Land annual snow accumulation variability is explored together with ice core chemistry data as proxies for circumpolar atmospheric circulation in the 110°E-135°E sector of the circumpolar trough. Four accumulation time series spanning 1930-1985 show a pattern of accumulation related to maritime air mass incursions over the East Antarctic ice sheet slope, which is regionally consistent on interannual and interdecadal timescales. The temporal accumulation pattern in Wilkes Land shows decadal fluctuations of ±10%. Both these fluctuations and the overall trend of increasing accumulation since the middle 1960s are consistent with a poleward shift and intensification of the circumpolar trough. This is consistent with a shift toward the high index state of the southern annular mode. Interannual variability of snow accumulation rate throughout Wilkes Land was found to be dependent upon shifts in the preferred tracks of cyclones along or across the coast and in the location of cyclolysis regions. Significant differences in this temporal accumulation pattern over Wilkes Land can occur as a result of the time-varying location of atmospheric ridging and the circumpolar long-wave structure south of New Zealand and Australia. Snow accumulation at an additional site (GD09) displays a well-defined interdecadal pattern, and the mean annual nitrate (NO-3) concentration of snow is correlated to the winter sea level pressure gradient between East Antarctica and the sub-Antarctic and the upper geopotential height and zonal wind data over East Antarctica. Strong, surface wind drainage during tropospheric ridging in Wilkes Land produces anomalous snow accumulation and annual mean NO-3 concentration in firn at GD09.
Affiliations:
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Pascal:04-0255816Le document en format XML
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De Angelis</name><affiliation wicri:level="3"><inist:fA14 i1="02"><s1>Laboratoire de Glaciologie et Géophysique de l'Environnement, CNRS</s1><s2>Saint Martin d'Hères</s2><s3>FRA</s3><sZ>2 aut.</sZ></inist:fA14><country>France</country><placeName><region type="region" nuts="2">Auvergne-Rhône-Alpes</region><region type="old region" nuts="2">Rhône-Alpes</region><settlement type="city">Saint-Martin-d'Hères</settlement><settlement type="city" wicri:auto="agglo">Grenoble</settlement></placeName></affiliation></author><author><name sortKey="Pook, M" sort="Pook, M" uniqKey="Pook M" first="M." last="Pook">M. Pook</name><affiliation wicri:level="1"><inist:fA14 i1="03"><s1>Antarctic Cooperative Research Centre, University of Tasmania</s1><s2>Hobart, Tasmania</s2><s3>AUS</s3><sZ>3 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Hobart, Tasmania</wicri:noRegion></affiliation></author><author><name sortKey="Young, N W" sort="Young, N W" uniqKey="Young N" first="N. 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Goodwin</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>School of Environmental and Life Sciences, University of Newcastle</s1><s2>Callaghan, NSW</s2><s3>AUS</s3><sZ>1 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Callaghan, NSW</wicri:noRegion></affiliation></author><author><name sortKey="De Angelis, M" sort="De Angelis, M" uniqKey="De Angelis M" first="M." last="De Angelis">M. De Angelis</name><affiliation wicri:level="3"><inist:fA14 i1="02"><s1>Laboratoire de Glaciologie et Géophysique de l'Environnement, CNRS</s1><s2>Saint Martin d'Hères</s2><s3>FRA</s3><sZ>2 aut.</sZ></inist:fA14><country>France</country><placeName><region type="region" nuts="2">Auvergne-Rhône-Alpes</region><region type="old region" nuts="2">Rhône-Alpes</region><settlement type="city">Saint-Martin-d'Hères</settlement><settlement type="city" wicri:auto="agglo">Grenoble</settlement></placeName></affiliation></author><author><name sortKey="Pook, M" sort="Pook, M" uniqKey="Pook M" first="M." last="Pook">M. Pook</name><affiliation wicri:level="1"><inist:fA14 i1="03"><s1>Antarctic Cooperative Research Centre, University of Tasmania</s1><s2>Hobart, Tasmania</s2><s3>AUS</s3><sZ>3 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Hobart, Tasmania</wicri:noRegion></affiliation></author><author><name sortKey="Young, N W" sort="Young, N W" uniqKey="Young N" first="N. W." last="Young">N. W. Young</name><affiliation wicri:level="1"><inist:fA14 i1="04"><s1>Antarctic Cooperative Research Centre and Australian Antarctic Division</s1><s2>Hobart, Tasmania</s2><s3>AUS</s3><sZ>4 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Antarctic Cooperative Research Centre and Australian Antarctic Division</wicri:noRegion></affiliation></author></analytic><series><title level="j" type="main">Journal of geophysical research</title><title level="j" type="abbreviated">J. geophys. res.</title><idno type="ISSN">0148-0227</idno><imprint><date when="2003">2003</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Journal of geophysical research</title><title level="j" type="abbreviated">J. geophys. res.</title><idno type="ISSN">0148-0227</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Accumulation rate</term><term>Air mass</term><term>Annular mode</term><term>Antarctica</term><term>Australia</term><term>Cyclolysis</term><term>Geopotential height</term><term>Intensification</term><term>Interannual variation</term><term>Ionospheric E region</term><term>Long wave</term><term>New Zealand</term><term>Pressure gradient</term><term>Snow accumulation</term><term>Surface wind</term><term>Time series</term><term>Winter</term><term>Zonal wind</term><term>annual variations</term><term>atmospheric circulation</term><term>drill cores</term><term>firn</term><term>fluctuations</term><term>ice sheets</term><term>sea level</term><term>snow</term><term>trajectory</term><term>troposphere</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Accumulation neige</term><term>Ionosphère région E</term><term>Variation annuelle</term><term>Carotte</term><term>Circulation atmosphérique</term><term>Série temporelle</term><term>Masse air</term><term>Inlandsis</term><term>Fluctuation</term><term>Intensification</term><term>Variation interannuelle</term><term>Taux accumulation</term><term>Trajectoire</term><term>Cyclolyse</term><term>Onde longue</term><term>Neige</term><term>Hiver</term><term>Niveau mer</term><term>Gradient pression</term><term>Hauteur géopotentielle</term><term>Antarctique</term><term>Nouvelle Zélande</term><term>Australie</term><term>Vent zonal</term><term>Vent surface</term><term>Troposphère</term><term>Névé</term><term>Mode annulaire</term></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Australie</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">[i] Wilkes Land annual snow accumulation variability is explored together with ice core chemistry data as proxies for circumpolar atmospheric circulation in the 110°E-135°E sector of the circumpolar trough. Four accumulation time series spanning 1930-1985 show a pattern of accumulation related to maritime air mass incursions over the East Antarctic ice sheet slope, which is regionally consistent on interannual and interdecadal timescales. The temporal accumulation pattern in Wilkes Land shows decadal fluctuations of ±10%. Both these fluctuations and the overall trend of increasing accumulation since the middle 1960s are consistent with a poleward shift and intensification of the circumpolar trough. This is consistent with a shift toward the high index state of the southern annular mode. Interannual variability of snow accumulation rate throughout Wilkes Land was found to be dependent upon shifts in the preferred tracks of cyclones along or across the coast and in the location of cyclolysis regions. Significant differences in this temporal accumulation pattern over Wilkes Land can occur as a result of the time-varying location of atmospheric ridging and the circumpolar long-wave structure south of New Zealand and Australia. Snow accumulation at an additional site (GD09) displays a well-defined interdecadal pattern, and the mean annual nitrate (NO<sup>-</sup>3) concentration of snow is correlated to the winter sea level pressure gradient between East Antarctica and the sub-Antarctic and the upper geopotential height and zonal wind data over East Antarctica. Strong, surface wind drainage during tropospheric ridging in Wilkes Land produces anomalous snow accumulation and annual mean NO<sup>-</sup>3 concentration in firn at GD09.</div></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0148-0227</s0></fA01><fA03 i2="1"><s0>J. geophys. res.</s0></fA03><fA05><s2>108</s2></fA05><fA06><s2>D21</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Snow accumulation variability in Wilkes land, East Antarctica, and the relationship to atmospheric ridging in the 130°-170°E region since 1930</s1></fA08><fA11 i1="01" i2="1"><s1>GOODWIN (I.)</s1></fA11><fA11 i1="02" i2="1"><s1>DE ANGELIS (M.)</s1></fA11><fA11 i1="03" i2="1"><s1>POOK (M.)</s1></fA11><fA11 i1="04" i2="1"><s1>YOUNG (N. W.)</s1></fA11><fA14 i1="01"><s1>School of Environmental and Life Sciences, University of Newcastle</s1><s2>Callaghan, NSW</s2><s3>AUS</s3><sZ>1 aut.</sZ></fA14><fA14 i1="02"><s1>Laboratoire de Glaciologie et Géophysique de l'Environnement, CNRS</s1><s2>Saint Martin d'Hères</s2><s3>FRA</s3><sZ>2 aut.</sZ></fA14><fA14 i1="03"><s1>Antarctic Cooperative Research Centre, University of Tasmania</s1><s2>Hobart, Tasmania</s2><s3>AUS</s3><sZ>3 aut.</sZ></fA14><fA14 i1="04"><s1>Antarctic Cooperative Research Centre and Australian Antarctic Division</s1><s2>Hobart, Tasmania</s2><s3>AUS</s3><sZ>4 aut.</sZ></fA14><fA20><s2>ACL6.1-ACL6.16</s2></fA20><fA21><s1>2003</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>3144</s2><s5>354000118984270050</s5></fA43><fA44><s0>0000</s0><s1>© 2004 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>51 ref.</s0></fA45><fA47 i1="01" i2="1"><s0>04-0255816</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Journal of geophysical research</s0></fA64><fA66 i1="01"><s0>USA</s0></fA66><fC01 i1="01" l="ENG"><s0>[i] Wilkes Land annual snow accumulation variability is explored together with ice core chemistry data as proxies for circumpolar atmospheric circulation in the 110°E-135°E sector of the circumpolar trough. Four accumulation time series spanning 1930-1985 show a pattern of accumulation related to maritime air mass incursions over the East Antarctic ice sheet slope, which is regionally consistent on interannual and interdecadal timescales. The temporal accumulation pattern in Wilkes Land shows decadal fluctuations of ±10%. Both these fluctuations and the overall trend of increasing accumulation since the middle 1960s are consistent with a poleward shift and intensification of the circumpolar trough. This is consistent with a shift toward the high index state of the southern annular mode. Interannual variability of snow accumulation rate throughout Wilkes Land was found to be dependent upon shifts in the preferred tracks of cyclones along or across the coast and in the location of cyclolysis regions. Significant differences in this temporal accumulation pattern over Wilkes Land can occur as a result of the time-varying location of atmospheric ridging and the circumpolar long-wave structure south of New Zealand and Australia. Snow accumulation at an additional site (GD09) displays a well-defined interdecadal pattern, and the mean annual nitrate (NO<sup>-</sup>3) concentration of snow is correlated to the winter sea level pressure gradient between East Antarctica and the sub-Antarctic and the upper geopotential height and zonal wind data over East Antarctica. Strong, surface wind drainage during tropospheric ridging in Wilkes Land produces anomalous snow accumulation and annual mean NO<sup>-</sup>3 concentration in firn at GD09.</s0></fC01><fC02 i1="01" i2="2"><s0>220</s0></fC02><fC02 i1="02" i2="3"><s0>001E</s0></fC02><fC03 i1="01" i2="X" l="FRE"><s0>Accumulation neige</s0><s5>26</s5></fC03><fC03 i1="01" i2="X" l="ENG"><s0>Snow accumulation</s0><s5>26</s5></fC03><fC03 i1="01" i2="X" l="SPA"><s0>Acumulación nieve</s0><s5>26</s5></fC03><fC03 i1="02" i2="X" l="FRE"><s0>Ionosphère région E</s0><s5>27</s5></fC03><fC03 i1="02" i2="X" l="ENG"><s0>Ionospheric E region</s0><s5>27</s5></fC03><fC03 i1="02" i2="X" l="SPA"><s0>Ionosfera región E</s0><s5>27</s5></fC03><fC03 i1="03" i2="2" l="FRE"><s0>Variation annuelle</s0><s5>28</s5></fC03><fC03 i1="03" i2="2" l="ENG"><s0>annual variations</s0><s5>28</s5></fC03><fC03 i1="03" i2="2" l="SPA"><s0>Variación anual</s0><s5>28</s5></fC03><fC03 i1="04" i2="2" l="FRE"><s0>Carotte</s0><s5>29</s5></fC03><fC03 i1="04" i2="2" l="ENG"><s0>drill cores</s0><s5>29</s5></fC03><fC03 i1="04" i2="2" l="SPA"><s0>Testigo</s0><s5>29</s5></fC03><fC03 i1="05" i2="2" l="FRE"><s0>Circulation atmosphérique</s0><s5>30</s5></fC03><fC03 i1="05" i2="2" l="ENG"><s0>atmospheric circulation</s0><s5>30</s5></fC03><fC03 i1="06" i2="X" l="FRE"><s0>Série temporelle</s0><s5>31</s5></fC03><fC03 i1="06" i2="X" l="ENG"><s0>Time series</s0><s5>31</s5></fC03><fC03 i1="06" i2="X" l="SPA"><s0>Serie temporal</s0><s5>31</s5></fC03><fC03 i1="07" i2="X" l="FRE"><s0>Masse air</s0><s5>32</s5></fC03><fC03 i1="07" i2="X" l="ENG"><s0>Air mass</s0><s5>32</s5></fC03><fC03 i1="07" i2="X" l="SPA"><s0>Masa aire</s0><s5>32</s5></fC03><fC03 i1="08" i2="2" l="FRE"><s0>Inlandsis</s0><s5>33</s5></fC03><fC03 i1="08" i2="2" l="ENG"><s0>ice sheets</s0><s5>33</s5></fC03><fC03 i1="08" i2="2" l="SPA"><s0>Masa de hielo</s0><s5>33</s5></fC03><fC03 i1="09" i2="2" l="FRE"><s0>Fluctuation</s0><s5>34</s5></fC03><fC03 i1="09" i2="2" 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l="SPA"><s0>Gradiente presión</s0><s5>44</s5></fC03><fC03 i1="20" i2="X" l="FRE"><s0>Hauteur géopotentielle</s0><s5>45</s5></fC03><fC03 i1="20" i2="X" l="ENG"><s0>Geopotential height</s0><s5>45</s5></fC03><fC03 i1="20" i2="X" l="SPA"><s0>Altura geopotencial</s0><s5>45</s5></fC03><fC03 i1="21" i2="2" l="FRE"><s0>Antarctique</s0><s2>NG</s2><s5>46</s5></fC03><fC03 i1="21" i2="2" l="ENG"><s0>Antarctica</s0><s2>NG</s2><s5>46</s5></fC03><fC03 i1="21" i2="2" l="SPA"><s0>Antártico</s0><s2>NG</s2><s5>46</s5></fC03><fC03 i1="22" i2="2" l="FRE"><s0>Nouvelle Zélande</s0><s2>NG</s2><s5>47</s5></fC03><fC03 i1="22" i2="2" l="ENG"><s0>New Zealand</s0><s2>NG</s2><s5>47</s5></fC03><fC03 i1="22" i2="2" l="SPA"><s0>Nueva Zelandia</s0><s2>NG</s2><s5>47</s5></fC03><fC03 i1="23" i2="2" l="FRE"><s0>Australie</s0><s2>NG</s2><s5>48</s5></fC03><fC03 i1="23" i2="2" l="ENG"><s0>Australia</s0><s2>NG</s2><s5>48</s5></fC03><fC03 i1="23" i2="2" l="SPA"><s0>Australia</s0><s2>NG</s2><s5>48</s5></fC03><fC03 i1="24" i2="X" l="FRE"><s0>Vent zonal</s0><s5>90</s5></fC03><fC03 i1="24" i2="X" l="ENG"><s0>Zonal wind</s0><s5>90</s5></fC03><fC03 i1="24" i2="X" l="SPA"><s0>Viento zonal</s0><s5>90</s5></fC03><fC03 i1="25" i2="X" l="FRE"><s0>Vent surface</s0><s5>91</s5></fC03><fC03 i1="25" i2="X" l="ENG"><s0>Surface wind</s0><s5>91</s5></fC03><fC03 i1="25" i2="X" l="SPA"><s0>Viento superficial</s0><s5>91</s5></fC03><fC03 i1="26" i2="2" l="FRE"><s0>Troposphère</s0><s5>92</s5></fC03><fC03 i1="26" i2="2" l="ENG"><s0>troposphere</s0><s5>92</s5></fC03><fC03 i1="27" i2="2" l="FRE"><s0>Névé</s0><s5>93</s5></fC03><fC03 i1="27" i2="2" l="ENG"><s0>firn</s0><s5>93</s5></fC03><fC03 i1="27" i2="2" l="SPA"><s0>Nevero</s0><s5>93</s5></fC03><fC03 i1="28" i2="2" l="FRE"><s0>Mode annulaire</s0><s4>CD</s4><s5>96</s5></fC03><fC03 i1="28" i2="2" l="ENG"><s0>Annular mode</s0><s4>CD</s4><s5>96</s5></fC03><fC03 i1="28" i2="2" l="SPA"><s0>Modo anular</s0><s4>CD</s4><s5>96</s5></fC03><fC07 i1="01" i2="2" l="FRE"><s0>Région Polaire</s0></fC07><fC07 i1="01" i2="2" l="ENG"><s0>polar regions</s0></fC07><fC07 i1="02" i2="2" l="FRE"><s0>Australasie</s0></fC07><fC07 i1="02" i2="2" l="ENG"><s0>Australasia</s0></fC07><fC07 i1="02" i2="2" l="SPA"><s0>Australasia</s0></fC07><fN21><s1>159</s1></fN21><fN82><s1>OTO</s1></fN82></pA></standard></inist><affiliations><list><country><li>Australie</li><li>France</li></country><region><li>Auvergne-Rhône-Alpes</li><li>Rhône-Alpes</li></region><settlement><li>Grenoble</li><li>Saint-Martin-d'Hères</li></settlement></list><tree><country name="Australie"><noRegion><name sortKey="Goodwin, I" sort="Goodwin, I" uniqKey="Goodwin I" first="I." last="Goodwin">I. Goodwin</name></noRegion><name sortKey="Pook, M" sort="Pook, M" uniqKey="Pook M" first="M." last="Pook">M. Pook</name><name sortKey="Young, N W" sort="Young, N W" uniqKey="Young N" first="N. W." last="Young">N. W. Young</name></country><country name="France"><region name="Auvergne-Rhône-Alpes"><name sortKey="De Angelis, M" sort="De Angelis, M" uniqKey="De Angelis M" first="M." last="De Angelis">M. De Angelis</name></region></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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|wiki= Wicri/Asie
|area= AustralieFrV1
|flux= PascalFrancis
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|texte= Snow accumulation variability in Wilkes land, East Antarctica, and the relationship to atmospheric ridging in the 130°-170°E region since 1930
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