The effect of slope aspect on the response of snowpack to climate warming in the Pyrenees
Identifieur interne : 000993 ( PascalFrancis/Curation ); précédent : 000992; suivant : 000994The effect of slope aspect on the response of snowpack to climate warming in the Pyrenees
Auteurs : J. I. Lopez-Moreno [Espagne] ; J. Revuelto [Espagne] ; M. Gilaberte [Espagne] ; E. Moran-Tejeda [Espagne] ; M. Pons [Andorre] ; E. Jover [Andorre] ; P. Esteban [Andorre] ; C. Garcia [Espagne] ; J. W. Pomeroy [Canada]Source :
- Theoretical and applied climatology [ 0177-798X ] ; 2014.
Descripteurs français
- Pascal (Inist)
- Wicri :
- topic : Changement climatique.
English descriptors
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Abstract
The aim of this study was to analyse the effect of slope aspect on the response of snowpack to climate warming in the Pyrenees. For this purpose, data available from five automatic weather stations were used to simulate the energy and mass balance of snowpack, assuming different magnitudes of an idealized climate warming (upward shifting of 1, 2 and 3 °C the temperature series). Snow energy and mass balance were simulated using the Cold Regions Hydrological Modelling platform (CRHM). CRHM was used to create a model that enabled correction of the all-wave incoming radiation fluxes from the observation sites for various slope aspects (N, NE, E, SE, S, SW,W,NW and flat areas), which enabled assessment of the differential impact of climate warming on snow processes on mountain slopes. The results showed that slope aspect was responsible for substantial variability in snow accumulation and the duration of the snowpack. Simulated variability markedly increased with warmer temperature conditions. Annual maximum snow accumulation (MSA) and annual snowpack duration (ASD) showed marked sensitivity to a warming of 1 °C. Thus, the sensitivity of the MSA in flat areas ranged from 11 to 17 % per degree C amongst the weather stations, and the ASD ranged from 11 to 20 days per degree C. There was a clear increase in the sensitivity of the snowpack to climate warming on those slopes that received intense solar radiation (S, SE and SW slopes) compared with those slopes where the incident radiation was more limited (N, NE and NW slopes). The sensitivity of the MSA and the ASD increased as the temperature increased, particularly on the most irradiated slopes. Large interannual variability was also observed. Thus, with more snow accumulation and longer duration the sensitivity of the snowpack to temperature decreased, especially on south-facing slopes.
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Pomeroy</name><affiliation wicri:level="1"><inist:fA14 i1="05"><s1>Center for Hydrology, University of Saskatchewan</s1><s2>Saskatoon, SK</s2><s3>CAN</s3><sZ>9 aut.</sZ></inist:fA14><country>Canada</country></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">14-0239501</idno><date when="2014">2014</date><idno type="stanalyst">PASCAL 14-0239501 INIST</idno><idno type="RBID">Pascal:14-0239501</idno><idno type="wicri:Area/PascalFrancis/Corpus">000011</idno><idno type="wicri:Area/PascalFrancis/Curation">000993</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">The effect of slope aspect on the response of snowpack to climate warming in the Pyrenees</title><author><name sortKey="Lopez Moreno, J I" sort="Lopez Moreno, J I" uniqKey="Lopez Moreno J" first="J. I." last="Lopez-Moreno">J. I. Lopez-Moreno</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Pyrenean Institute of Ecology (CSIC), Avda. Montañana 1005</s1><s2>Zaragoza 50 059</s2><s3>ESP</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ><sZ>4 aut.</sZ></inist:fA14><country>Espagne</country></affiliation></author><author><name sortKey="Revuelto, J" sort="Revuelto, J" uniqKey="Revuelto J" first="J." last="Revuelto">J. Revuelto</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Pyrenean Institute of Ecology (CSIC), Avda. Montañana 1005</s1><s2>Zaragoza 50 059</s2><s3>ESP</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ><sZ>4 aut.</sZ></inist:fA14><country>Espagne</country></affiliation></author><author><name sortKey="Gilaberte, M" sort="Gilaberte, M" uniqKey="Gilaberte M" first="M." last="Gilaberte">M. Gilaberte</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Pyrenean Institute of Ecology (CSIC), Avda. Montañana 1005</s1><s2>Zaragoza 50 059</s2><s3>ESP</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ><sZ>4 aut.</sZ></inist:fA14><country>Espagne</country></affiliation></author><author><name sortKey="Moran Tejeda, E" sort="Moran Tejeda, E" uniqKey="Moran Tejeda E" first="E." last="Moran-Tejeda">E. Moran-Tejeda</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Pyrenean Institute of Ecology (CSIC), Avda. Montañana 1005</s1><s2>Zaragoza 50 059</s2><s3>ESP</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ><sZ>4 aut.</sZ></inist:fA14><country>Espagne</country></affiliation></author><author><name sortKey="Pons, M" sort="Pons, M" uniqKey="Pons M" first="M." last="Pons">M. Pons</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Observatory of Sustainability of Andorra (OBSA)</s1><s2>Sant Julià de Lòria</s2><s3>AND</s3><sZ>5 aut.</sZ><sZ>6 aut.</sZ></inist:fA14><country>Andorre</country></affiliation></author><author><name sortKey="Jover, E" sort="Jover, E" uniqKey="Jover E" first="E." last="Jover">E. Jover</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Observatory of Sustainability of Andorra (OBSA)</s1><s2>Sant Julià de Lòria</s2><s3>AND</s3><sZ>5 aut.</sZ><sZ>6 aut.</sZ></inist:fA14><country>Andorre</country></affiliation></author><author><name sortKey="Esteban, P" sort="Esteban, P" uniqKey="Esteban P" first="P." last="Esteban">P. Esteban</name><affiliation wicri:level="1"><inist:fA14 i1="03"><s1>Centre d'estudis de la neu i de la muntanya d'Andorra (CENMA)</s1><s2>Sant Julià de Lòria</s2><s3>AND</s3><sZ>7 aut.</sZ></inist:fA14><country>Andorre</country></affiliation></author><author><name sortKey="Garcia, C" sort="Garcia, C" uniqKey="Garcia C" first="C." last="Garcia">C. Garcia</name><affiliation wicri:level="1"><inist:fA14 i1="04"><s1>Geological Institute of Cataluña (IGC)</s1><s2>Barcelona</s2><s3>ESP</s3><sZ>8 aut.</sZ></inist:fA14><country>Espagne</country></affiliation></author><author><name sortKey="Pomeroy, J W" sort="Pomeroy, J W" uniqKey="Pomeroy J" first="J. W." last="Pomeroy">J. W. Pomeroy</name><affiliation wicri:level="1"><inist:fA14 i1="05"><s1>Center for Hydrology, University of Saskatchewan</s1><s2>Saskatoon, SK</s2><s3>CAN</s3><sZ>9 aut.</sZ></inist:fA14><country>Canada</country></affiliation></author></analytic><series><title level="j" type="main">Theoretical and applied climatology</title><title level="j" type="abbreviated">Theor. appl. climatol.</title><idno type="ISSN">0177-798X</idno><imprint><date when="2014">2014</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Theoretical and applied climatology</title><title level="j" type="abbreviated">Theor. appl. climatol.</title><idno type="ISSN">0177-798X</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Atmosphere cryosphere interaction</term><term>Interannual variation</term><term>Pyrenees</term><term>Snow cover</term><term>climate change</term><term>climate warming</term><term>digital simulation</term><term>energy balance</term><term>global change</term><term>mass balance</term><term>sensitivity analysis</term><term>slopes</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Couverture neige</term><term>Interaction atmosphère cryosphère</term><term>Réchauffement climat</term><term>Changement planétaire</term><term>Changement climatique</term><term>Versant</term><term>Bilan masse</term><term>Bilan énergie</term><term>Variation interannuelle</term><term>Simulation numérique</term><term>Analyse sensibilité</term><term>Pyrénées</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Changement climatique</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The aim of this study was to analyse the effect of slope aspect on the response of snowpack to climate warming in the Pyrenees. For this purpose, data available from five automatic weather stations were used to simulate the energy and mass balance of snowpack, assuming different magnitudes of an idealized climate warming (upward shifting of 1, 2 and 3 °C the temperature series). Snow energy and mass balance were simulated using the Cold Regions Hydrological Modelling platform (CRHM). CRHM was used to create a model that enabled correction of the all-wave incoming radiation fluxes from the observation sites for various slope aspects (N, NE, E, SE, S, SW,W,NW and flat areas), which enabled assessment of the differential impact of climate warming on snow processes on mountain slopes. The results showed that slope aspect was responsible for substantial variability in snow accumulation and the duration of the snowpack. Simulated variability markedly increased with warmer temperature conditions. Annual maximum snow accumulation (MSA) and annual snowpack duration (ASD) showed marked sensitivity to a warming of 1 °C. Thus, the sensitivity of the MSA in flat areas ranged from 11 to 17 % per degree C amongst the weather stations, and the ASD ranged from 11 to 20 days per degree C. There was a clear increase in the sensitivity of the snowpack to climate warming on those slopes that received intense solar radiation (S, SE and SW slopes) compared with those slopes where the incident radiation was more limited (N, NE and NW slopes). The sensitivity of the MSA and the ASD increased as the temperature increased, particularly on the most irradiated slopes. Large interannual variability was also observed. Thus, with more snow accumulation and longer duration the sensitivity of the snowpack to temperature decreased, especially on south-facing slopes.</div></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0177-798X</s0></fA01><fA03 i2="1"><s0>Theor. appl. climatol.</s0></fA03><fA05><s2>117</s2></fA05><fA06><s2>1-2</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>The effect of slope aspect on the response of snowpack to climate warming in the Pyrenees</s1></fA08><fA11 i1="01" i2="1"><s1>LOPEZ-MORENO (J. I.)</s1></fA11><fA11 i1="02" i2="1"><s1>REVUELTO (J.)</s1></fA11><fA11 i1="03" i2="1"><s1>GILABERTE (M.)</s1></fA11><fA11 i1="04" i2="1"><s1>MORAN-TEJEDA (E.)</s1></fA11><fA11 i1="05" i2="1"><s1>PONS (M.)</s1></fA11><fA11 i1="06" i2="1"><s1>JOVER (E.)</s1></fA11><fA11 i1="07" i2="1"><s1>ESTEBAN (P.)</s1></fA11><fA11 i1="08" i2="1"><s1>GARCIA (C.)</s1></fA11><fA11 i1="09" i2="1"><s1>POMEROY (J. W.)</s1></fA11><fA14 i1="01"><s1>Pyrenean Institute of Ecology (CSIC), Avda. Montañana 1005</s1><s2>Zaragoza 50 059</s2><s3>ESP</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ><sZ>4 aut.</sZ></fA14><fA14 i1="02"><s1>Observatory of Sustainability of Andorra (OBSA)</s1><s2>Sant Julià de Lòria</s2><s3>AND</s3><sZ>5 aut.</sZ><sZ>6 aut.</sZ></fA14><fA14 i1="03"><s1>Centre d'estudis de la neu i de la muntanya d'Andorra (CENMA)</s1><s2>Sant Julià de Lòria</s2><s3>AND</s3><sZ>7 aut.</sZ></fA14><fA14 i1="04"><s1>Geological Institute of Cataluña (IGC)</s1><s2>Barcelona</s2><s3>ESP</s3><sZ>8 aut.</sZ></fA14><fA14 i1="05"><s1>Center for Hydrology, University of Saskatchewan</s1><s2>Saskatoon, SK</s2><s3>CAN</s3><sZ>9 aut.</sZ></fA14><fA20><s1>207-219</s1></fA20><fA21><s1>2014</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>2172B</s2><s5>354000507626410160</s5></fA43><fA44><s0>0000</s0><s1>© 2014 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>1 p.1/4</s0></fA45><fA47 i1="01" i2="1"><s0>14-0239501</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Theoretical and applied climatology</s0></fA64><fA66 i1="01"><s0>AUT</s0></fA66><fC01 i1="01" l="ENG"><s0>The aim of this study was to analyse the effect of slope aspect on the response of snowpack to climate warming in the Pyrenees. For this purpose, data available from five automatic weather stations were used to simulate the energy and mass balance of snowpack, assuming different magnitudes of an idealized climate warming (upward shifting of 1, 2 and 3 °C the temperature series). Snow energy and mass balance were simulated using the Cold Regions Hydrological Modelling platform (CRHM). CRHM was used to create a model that enabled correction of the all-wave incoming radiation fluxes from the observation sites for various slope aspects (N, NE, E, SE, S, SW,W,NW and flat areas), which enabled assessment of the differential impact of climate warming on snow processes on mountain slopes. The results showed that slope aspect was responsible for substantial variability in snow accumulation and the duration of the snowpack. Simulated variability markedly increased with warmer temperature conditions. Annual maximum snow accumulation (MSA) and annual snowpack duration (ASD) showed marked sensitivity to a warming of 1 °C. Thus, the sensitivity of the MSA in flat areas ranged from 11 to 17 % per degree C amongst the weather stations, and the ASD ranged from 11 to 20 days per degree C. There was a clear increase in the sensitivity of the snowpack to climate warming on those slopes that received intense solar radiation (S, SE and SW slopes) compared with those slopes where the incident radiation was more limited (N, NE and NW slopes). The sensitivity of the MSA and the ASD increased as the temperature increased, particularly on the most irradiated slopes. Large interannual variability was also observed. 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