RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES
Identifieur interne : 001672 ( Istex/Corpus ); précédent : 001671; suivant : 001673RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES
Auteurs : T. Chinn ; S. Winkler ; M. J. Salinger ; N. HaakensenSource :
- Geografiska Annaler: Series A, Physical Geography [ 0435-3676 ] ; 2005-03.
English descriptors
- KwdEn :
- ENSO/SOI, IPO, NAO, New Zealand, Norway, advance, glaciers, mass balance.
Abstract
ABSTRACT. Norway and New Zealand both experienced recent glacial advances, commencing in the early 1980s and ceasing around 2000, which were more extensive than any other since the end of the Little Ice Age. Common to both countries, the positive glacier balances are associated with an increase in the strength of westerly atmospheric circulation which brought increased precipitation. In Norway, the changes are also associated with lower ablation season temperatures. In New Zealand, where the positive balances were distributed uniformly throughout the Southern Alps, the period of increased mass balance was coincident with a change in the Interdecadal Pacific Oscillation and an associated increase in El Niño/Southern Oscillation events. In Norway, the positive balances occurred across a strong west‐east gradient with no balance increases to the continental glaciers of Scandinavia. The Norwegian advances are linked to strongly positive North Atlantic Oscillation events which caused an overall increase of precipitation in the winter accumulation season and a general shift of maximum precipitation from autumn towards winter. These cases both show the influence of atmospheric circulation on maritime glaciers.
Url:
DOI: 10.1111/j.0435-3676.2005.00249.x
Links to Exploration step
ISTEX:854CD15ED50A44B84B705B93B1D01BB74A0BA51DLe document en format XML
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Winkler</name><affiliation><mods:affiliation>Department of Geography, University of Würzburg, Würzburg, Germany</mods:affiliation></affiliation><affiliation><mods:affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</mods:affiliation></affiliation></author><author><name sortKey="Salinger, M J" sort="Salinger, M J" uniqKey="Salinger M" first="M. J." last="Salinger">M. J. Salinger</name><affiliation><mods:affiliation>National Institute of Water and Atmospheric Research, Auckland, New Zealand</mods:affiliation></affiliation><affiliation><mods:affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</mods:affiliation></affiliation></author><author><name sortKey="Haakensen, N" sort="Haakensen, N" uniqKey="Haakensen N" first="N." last="Haakensen">N. Haakensen</name><affiliation><mods:affiliation>Norwegian Water Resources and Energy Directorate (NVE), Oslo, Norway</mods:affiliation></affiliation><affiliation><mods:affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:854CD15ED50A44B84B705B93B1D01BB74A0BA51D</idno><date when="2005" year="2005">2005</date><idno type="doi">10.1111/j.0435-3676.2005.00249.x</idno><idno type="url">https://api.istex.fr/document/854CD15ED50A44B84B705B93B1D01BB74A0BA51D/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">001672</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001672</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES</title><author><name sortKey="Chinn, T" sort="Chinn, T" uniqKey="Chinn T" first="T." last="Chinn">T. Chinn</name><affiliation><mods:affiliation>Lake Hawea, Wanaka, Otago, New Zealand</mods:affiliation></affiliation><affiliation><mods:affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</mods:affiliation></affiliation></author><author><name sortKey="Winkler, S" sort="Winkler, S" uniqKey="Winkler S" first="S." last="Winkler">S. Winkler</name><affiliation><mods:affiliation>Department of Geography, University of Würzburg, Würzburg, Germany</mods:affiliation></affiliation><affiliation><mods:affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</mods:affiliation></affiliation></author><author><name sortKey="Salinger, M J" sort="Salinger, M J" uniqKey="Salinger M" first="M. J." last="Salinger">M. J. Salinger</name><affiliation><mods:affiliation>National Institute of Water and Atmospheric Research, Auckland, New Zealand</mods:affiliation></affiliation><affiliation><mods:affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</mods:affiliation></affiliation></author><author><name sortKey="Haakensen, N" sort="Haakensen, N" uniqKey="Haakensen N" first="N." last="Haakensen">N. Haakensen</name><affiliation><mods:affiliation>Norwegian Water Resources and Energy Directorate (NVE), Oslo, Norway</mods:affiliation></affiliation><affiliation><mods:affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Geografiska Annaler: Series A, Physical Geography</title><idno type="ISSN">0435-3676</idno><idno type="eISSN">1468-0459</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><date type="published" when="2005-03">2005-03</date><biblScope unit="volume">87</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="141">141</biblScope><biblScope unit="page" to="157">157</biblScope></imprint><idno type="ISSN">0435-3676</idno></series><idno type="istex">854CD15ED50A44B84B705B93B1D01BB74A0BA51D</idno><idno type="DOI">10.1111/j.0435-3676.2005.00249.x</idno><idno type="ArticleID">GEOA249</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0435-3676</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>ENSO/SOI</term><term>IPO</term><term>NAO</term><term>New Zealand</term><term>Norway</term><term>advance</term><term>glaciers</term><term>mass balance</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">ABSTRACT. Norway and New Zealand both experienced recent glacial advances, commencing in the early 1980s and ceasing around 2000, which were more extensive than any other since the end of the Little Ice Age. Common to both countries, the positive glacier balances are associated with an increase in the strength of westerly atmospheric circulation which brought increased precipitation. In Norway, the changes are also associated with lower ablation season temperatures. In New Zealand, where the positive balances were distributed uniformly throughout the Southern Alps, the period of increased mass balance was coincident with a change in the Interdecadal Pacific Oscillation and an associated increase in El Niño/Southern Oscillation events. In Norway, the positive balances occurred across a strong west‐east gradient with no balance increases to the continental glaciers of Scandinavia. The Norwegian advances are linked to strongly positive North Atlantic Oscillation events which caused an overall increase of precipitation in the winter accumulation season and a general shift of maximum precipitation from autumn towards winter. These cases both show the influence of atmospheric circulation on maritime glaciers.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>T. CHINN</name><affiliations><json:string>Lake Hawea, Wanaka, Otago, New Zealand</json:string><json:string>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</json:string></affiliations></json:item><json:item><name>S. WINKLER</name><affiliations><json:string>Department of Geography, University of Würzburg, Würzburg, Germany</json:string><json:string>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</json:string></affiliations></json:item><json:item><name>M.J. SALINGER</name><affiliations><json:string>National Institute of Water and Atmospheric Research, Auckland, New Zealand</json:string><json:string>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</json:string></affiliations></json:item><json:item><name>N. HAAKENSEN</name><affiliations><json:string>Norwegian Water Resources and Energy Directorate (NVE), Oslo, Norway</json:string><json:string>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>glaciers</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>mass balance</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>advance</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>NAO</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>IPO</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>ENSO/SOI</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Norway</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>New Zealand</value></json:item></subject><articleId><json:string>GEOA249</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>ABSTRACT. Norway and New Zealand both experienced recent glacial advances, commencing in the early 1980s and ceasing around 2000, which were more extensive than any other since the end of the Little Ice Age. Common to both countries, the positive glacier balances are associated with an increase in the strength of westerly atmospheric circulation which brought increased precipitation. In Norway, the changes are also associated with lower ablation season temperatures. In New Zealand, where the positive balances were distributed uniformly throughout the Southern Alps, the period of increased mass balance was coincident with a change in the Interdecadal Pacific Oscillation and an associated increase in El Niño/Southern Oscillation events. In Norway, the positive balances occurred across a strong west‐east gradient with no balance increases to the continental glaciers of Scandinavia. The Norwegian advances are linked to strongly positive North Atlantic Oscillation events which caused an overall increase of precipitation in the winter accumulation season and a general shift of maximum precipitation from autumn towards winter. These cases both show the influence of atmospheric circulation on maritime glaciers.</abstract><qualityIndicators><score>7.124</score><pdfVersion>1.3</pdfVersion><pdfPageSize>468 x 683 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>1222</abstractCharCount><pdfWordCount>8624</pdfWordCount><pdfCharCount>54874</pdfCharCount><pdfPageCount>17</pdfPageCount><abstractWordCount>177</abstractWordCount></qualityIndicators><title>RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES</title><refBibs><json:item><host><author></author><title>The response of Franz Josef Glacier to climate changePhD thesis</title></host></json:item><json:item><author><json:item><name>P.W. Anderton</name></json:item><json:item><name>T.J. Chinn</name></json:item></author><host><volume>20</volume><pages><last>84</last><first>67</first></pages><author></author><title>Journal of Glaciology</title></host><title>Ivory Glacier, New Zealand, an I.H.D. representative basin study</title></json:item><json:item><author><json:item><name>C. Appenzeller</name></json:item><json:item><name>T.F. Stacker</name></json:item><json:item><name>M. Anklin</name></json:item></author><host><volume>282</volume><pages><last>449</last><first>446</first></pages><author></author><title>Science</title></host><title>North Atlantic Oscillation dynamics recorded in Greenland ice cores</title></json:item><json:item><author><json:item><name>C.K. Ballantyne</name></json:item></author><host><volume>19</volume><pages><last>117</last><first>93</first></pages><author></author><title>Boreas</title></host><title>The Holocene glacial history of Lyngshalvöya, northern Norway: chronology and climatic implications</title></json:item><json:item><author><json:item><name>R. W. Bickerton</name></json:item><json:item><name>J.A. Matthews</name></json:item></author><host><volume>8</volume><pages><last>66</last><first>45</first></pages><author></author><title>Journal of Quaternary Science</title></host><title>Variations of outlet glaciers from the Jostedalsbreen ice‐cap, southern Norway: a regional lichenometric‐dating study of ice‐marginal moraine sequences and their climatic significance</title></json:item><json:item><author><json:item><name>J. Bogen</name></json:item><json:item><name>B. Wold</name></json:item><json:item><name>G. Østrem</name></json:item></author><host><pages><last>128</last><first>109</first></pages><author></author><title>Glacier Fluctuations and Climatic Change</title></host><title>Historic glacier variations in Scandinavia</title></json:item><json:item><author><json:item><name>T.J.H. Chinn</name></json:item></author><host><volume>27</volume><pages><last>198</last><first>187</first></pages><author></author><title>Arctic and Alpine Research</title></host><title>Glacier fluctuations in the Southern Alps of New Zealand determined from snowline elevation</title></json:item><json:item><author><json:item><name>T.J.H. Chinn</name></json:item></author><host><volume>39</volume><pages><last>428</last><first>415</first></pages><author></author><title>New Zealand Journal of Geology and Geophysics</title></host><title>New Zealand glacier responses to climate change of the past century</title></json:item><json:item><author><json:item><name>T.J.H. Chinn</name></json:item></author><host><volume>22</volume><pages><last>168</last><first>155</first></pages><author></author><title>Global and Planetary Change</title></host><title>New Zealand glacier response to climate change of the past 2 decades</title></json:item><json:item><author><json:item><name>T.J.H. Chinn</name></json:item></author><host><volume>40</volume><pages><last>187</last><first>139</first></pages><issue>2</issue><author></author><title>Journal of Hydrology (NZ)</title></host><title>Distribution of the glacial water resources of New Zealand</title></json:item><json:item><host><author></author><title>New Zealand glacier snowline survey</title></host></json:item><json:item><author><json:item><name>T.J. Chinn</name></json:item><json:item><name>C. Heydenrych</name></json:item><json:item><name>M.J. Salinger</name></json:item></author><host><author></author><title>Journal of Glaciology.</title></host><title>Use of the ELA as a practical method of monitoring glacier response to climate in the New Zealand's Southern Alps</title></json:item><json:item><author><json:item><name>G.R. Clare</name></json:item><json:item><name>B.B. Fitzharris</name></json:item><json:item><name>T.J.H. Chinn</name></json:item><json:item><name>M.J. Salinger</name></json:item></author><host><volume>22</volume><pages><last>120</last><first>107</first></pages><author></author><title>International Journal of Climate</title></host><title>Variation in end‐of‐summer snowlines of the Southern Alps of New Zealand, and relationships with Southern Hemisphere atmospheric circulation and sea surface temperature patterns</title></json:item><json:item><author><json:item><name>E.R. Cook</name></json:item><json:item><name>R.D. D'Arrigo</name></json:item><json:item><name>K.R. Briffa</name></json:item></author><host><volume>8</volume><pages><last>17</last><first>9</first></pages><author></author><title>The Holocene</title></host><title>A reconstruction of the North Atlantic Oscillation using tree‐ring chronologies from North America and Europe</title></json:item><json:item><author><json:item><name>J.A. Dowdeswell</name></json:item><json:item><name>J.O. Hagen</name></json:item><json:item><name>H. Bjørnsson</name></json:item><json:item><name>A.F. Glazovsky</name></json:item><json:item><name>W.D. Harrison</name></json:item><json:item><name>P. Holmlund</name></json:item><json:item><name>J. Jania</name></json:item><json:item><name>R.M. Koerner</name></json:item><json:item><name>B. Le‐fauconnier</name></json:item><json:item><name>C.S.L. Ommanney</name></json:item><json:item><name>R.H. Thomas</name></json:item></author><host><volume>48</volume><pages><last>14</last><first>1</first></pages><author></author><title>Quaternary Research</title></host><title>The mass balance of circum‐Arctic glaciers and recent climate change</title></json:item><json:item><author><json:item><name>L. Erikstad</name></json:item><json:item><name>J.L. Sollid</name></json:item></author><host><volume>40</volume><pages><last>100</last><first>85</first></pages><author></author><title>Norsk Geografisk Tidskrift</title></host><title>Neoglaciation in South Norway using lichenometric methods</title></json:item><json:item><author><json:item><name>K. Fœgri</name></json:item></author><host><volume>7</volume><pages><first>255</first></pages><author></author><title>Bergens Museums Årbok 1933 Naturvidenskapelig rekke</title></host><title>Über die Längenvariationen einiger Gletscher des Jostedalsbre und die dadurch bedingten Pflanzensukzessionen</title></json:item><json:item><author><json:item><name>K. Fœgri</name></json:item></author><host><volume>72</volume><pages><last>243</last><first>230</first></pages><author></author><title>Na-turen</title></host><title>Brevariasjoner i Vestnorge i de siste 200 år</title></json:item><json:item><author><json:item><name>B.B. Fitzharris</name></json:item><json:item><name>J.E. Hay</name></json:item><json:item><name>P.O. Jones</name></json:item></author><host><volume>2</volume><pages><last>106</last><first>97</first></pages><author></author><title>The Holocene</title></host><title>Behaviour of New Zealand glaciers and atmospheric circulation changes over the past 130 years</title></json:item><json:item><author><json:item><name>B.B. Fitzharris</name></json:item><json:item><name>T.J.H. Chinn</name></json:item><json:item><name>G.N. Lament</name></json:item></author><host><volume>17</volume><pages><last>763</last><first>745</first></pages><author></author><title>International Journal of Climate</title></host><title>Glacier balance fluctuations and atmospheric circulation patterns over the Southern Alps, New Zealand</title></json:item><json:item><host><author></author><title>Nedbørnormaler normalperiode 1961–1990</title></host></json:item><json:item><author><json:item><name>E.J. Førland</name></json:item><json:item><name>I. Hanssen‐Bauer</name></json:item><json:item><name>P.Ø. Nordli</name></json:item></author><host><volume>46</volume><pages><last>94</last><first>83</first></pages><author></author><title>Norsk Geografisk Tidskrift</title></host><title>New Norwegian climate normals – but has the climate changed</title></json:item><json:item><author><json:item><name>A.F. Gellatly</name></json:item></author><host><volume>151</volume><pages><last>99</last><first>86</first></pages><author></author><title>Geographical Journal</title></host><title>Historical records of glacier fluctuations in Mt Cook National Park, New Zealand: a century of change</title></json:item><json:item><author><json:item><name>A.F. Gellatly</name></json:item><json:item><name>T.J.H. Chinn</name></json:item><json:item><name>P. Röthlisberger</name></json:item></author><host><volume>7</volume><pages><last>242</last><first>227</first></pages><author></author><title>Quaternary Science Reviews</title></host><title>Holocene glacier variations in New Zealand: a review</title></json:item><json:item><author><json:item><name>N.J. Griffey</name></json:item><json:item><name>P. Worsley</name></json:item></author><host><volume>7</volume><pages><last>17</last><first>1</first></pages><author></author><title>Boreas</title></host><title>The pattern of Neoglacial glacier variations in the Okstindan region of northern Norway during the last three millennia</title></json:item><json:item><author><json:item><name>G.A. Griffiths</name></json:item><json:item><name>M.J. McSaveney</name></json:item></author><host><volume>26</volume><pages><last>209</last><first>197</first></pages><author></author><title>New Zealand Journal of Science</title></host><title>Distribution of mean annual precipitation across some steep‐land regions of New Zealand</title></json:item><json:item><host><pages><first>498</first></pages><author></author><title>Grove, J.M., 1988: The Little Ice Age. Routledge. London and New York . 498p.</title></host></json:item><json:item><author><json:item><name>N. Haakensen</name></json:item></author><host><volume>13</volume><pages><last>94</last><first>91</first></pages><author></author><title>Vœret</title></host><title>Akkumulasjon på breene i Norge vinteren 988‐89</title></json:item><json:item><author><json:item><name>W. Haeberli</name></json:item><json:item><name>M. Hoelzle</name></json:item></author><host><volume>21</volume><pages><last>212</last><first>206</first></pages><author></author><title>Annals of Glaciology</title></host><title>Application of inventory data for estimating characteristics of and regional climate‐change effects on mountain glaciers: a pilot study with the European Alps</title></json:item><json:item><author><json:item><name>W. Haeberli</name></json:item><json:item><name>R. Frauenfelder</name></json:item><json:item><name>M. Hoelzle</name></json:item><json:item><name>M. Maisch</name></json:item></author><host><volume>81A</volume><pages><last>591</last><first>585</first></pages><author></author><title>Geografiska Annaler</title></host><title>On rates and acceleration trends of global glacier mass changes</title></json:item><json:item><author><json:item><name>J.E. Hay</name></json:item><json:item><name>B.B. Fitzharris</name></json:item></author><host><volume>8</volume><pages><last>215</last><first>201</first></pages><author></author><title>International Journal of Climate</title></host><title>The synoptic climatology of ablation on a New Zealand glacier</title></json:item><json:item><author><json:item><name>J.W.D. Hessell</name></json:item></author><host><volume>23</volume><pages><last>9</last><first>1</first></pages><author></author><title>New Zealand Journal of Science</title></host><title>Apparent trends of mean temperature in New Zealand since 1930</title></json:item><json:item><author><json:item><name>J.W.D. Hessell</name></json:item></author><host><volume>26</volume><pages><last>320</last><first>315</first></pages><author></author><title>New Zealand Journal of Science</title></host><title>Climatic effects on the recession of the Franz Josef Glacier</title></json:item><json:item><author><json:item><name>A. Hoel</name></json:item><json:item><name>W. Werenskiold</name></json:item></author><host><volume>114</volume><pages><first>291</first></pages><author></author><title>Norsk Polarinstitutt Skrifter</title></host><title>Glaciers and snowfields in Norway</title></json:item><json:item><author><json:item><name>B.L. Hooker</name></json:item><json:item><name>B.B. Fitzharris</name></json:item></author><host><volume>22</volume><pages><last>48</last><first>39</first></pages><author></author><title>Global and Planetary Change</title></host><title>The correlation between climatic parameters and the retreat and advance of Franz Josef Glacier, New Zealand</title></json:item><json:item><author><json:item><name>J. W. Hurrel</name></json:item></author><host><volume>269</volume><pages><last>679</last><first>676</first></pages><author></author><title>Science</title></host><title>Decadal trends in the North Atlantic Oscillation: regional temperatures and precipitations</title></json:item><json:item><host><pages><first>881</first></pages><author></author><title>IPCC, 2001: Climate Change2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. In: Houghton, J.T., Ding, Y., Griggs, D.J., Noguer, M., Van der Linden, P.J., Dai, X., Maskell, K., and Johnson, C.A., (eds): Cambridge University Press. Cambridge . 881p.</title></host></json:item><json:item><author><json:item><name>T. Jóhannesson</name></json:item><json:item><name>O. Sigurdsson</name></json:item><json:item><name>T. Laumann</name></json:item><json:item><name>M. Kennett</name></json:item></author><host><volume>41</volume><pages><last>358</last><first>345</first></pages><author></author><title>Journal of Glaciology</title></host><title>Degree‐day glacier mass‐balance modelling with applications to glaciers in Iceland, Norway and Greenland</title></json:item><json:item><author><json:item><name>W. Karlén</name></json:item></author><host><volume>61A</volume><pages><last>28</last><first>11</first></pages><author></author><title>Geografiska Annaler</title></host><title>Glacier variations in the Svartisen area, Northern Norway</title></json:item><json:item><author><json:item><name>M. Kirkbride</name></json:item></author><host><volume>3</volume><pages><last>240</last><first>232</first></pages><author></author><title>The Holocene</title></host><title>The temporal significance of transitions from melting to calving termini at glaciers in the central Southern Alps of New Zealand</title></json:item><json:item><author><json:item><name>M.P. Kirkbride</name></json:item><json:item><name>C.R. Warren</name></json:item></author><host><volume>24</volume><pages><last>121</last><first>116</first></pages><author></author><title>Annals of Glaciology</title></host><title>Calving processes at a grounded ice cliff</title></json:item><json:item><host><author></author><title>Glasiologiske undersøkelser i Norge 1999</title></host></json:item><json:item><host><author></author><title>Regional breovervaking i Sør‐Norge</title></host></json:item><json:item><author><json:item><name>M. Kuhn</name></json:item></author><host><volume>22</volume><pages><last>272</last><first>263</first></pages><author></author><title>Journal of Glaciology</title></host><title>On the computation of heat transfer coefficients from energy‐balance gradients on a glacier</title></json:item><json:item><author><json:item><name>P.J. Lamb</name></json:item><json:item><name>R.A. Peppier</name></json:item></author><host><volume>68</volume><pages><last>1225</last><first>1218</first></pages><author></author><title>Bulletin of the American Meteorological Society</title></host><title>North Atlantic Oscillation: concept and an application</title></json:item><json:item><author><json:item><name>G.N. Lament</name></json:item><json:item><name>T.J.H. Cham</name></json:item><json:item><name>B.B. Fitzharris</name></json:item></author><host><volume>22</volume><pages><last>219</last><first>209</first></pages><author></author><title>Global Planetary Change</title></host><title>Slopes of ELAs in the Southern Alps of New Zealand in relation to atmospheric circulation patterns</title></json:item><json:item><author><json:item><name>T. Laumann</name></json:item><json:item><name>N. Reeh</name></json:item></author><host><volume>39</volume><pages><last>665</last><first>656</first></pages><author></author><title>Journal of Glaciology</title></host><title>Sensitivity to climate change of the mass balance of glaciers in southern Norway</title></json:item><json:item><author><json:item><name>D.B. Lawrence</name></json:item><json:item><name>E.G. Lawrence</name></json:item></author><host><volume>47</volume><pages><last>27</last><first>17</first></pages><author></author><title>Manama</title></host><title>Glacier studies in New Zealand</title></json:item><json:item><author><json:item><name>O. Liestøl</name></json:item></author><host><volume>141</volume><pages><first>63</first></pages><author></author><title>Jotunheimen. Norsk Polarinstitutt Skrifter</title></host><title>Storbreen glacier in</title></json:item><json:item><author><json:item><name>J.A. Matthews</name></json:item><json:item><name>R.A. Shakesby</name></json:item></author><host><volume>13</volume><pages><last>346</last><first>333</first></pages><author></author><title>Boreas</title></host><title>The status of the ‘Little Ice Age’ in southern Norway: relative‐age dating of Neoglacial moraines with Schmidt hammer and lichenometry</title></json:item><json:item><author><json:item><name>A.B. Mutton</name></json:item></author><host><volume>15</volume><pages><last>1386</last><first>1365</first></pages><author></author><title>International Journal of Climate</title></host><title>On the linearity and stability of Southern Oscillation‐climate relationships for New Zealand</title></json:item><json:item><author><json:item><name>A. Nesje</name></json:item></author><host><volume>43</volume><pages><last>17</last><first>3</first></pages><author></author><title>Norsk Geografisk Tid-skrift</title></host><title>Glacier‐front variations at the outlet glaciers from Jostedalsbreen and climate in the Jostedalsbre region of western Norway in the period 1901–1980</title></json:item><json:item><author><json:item><name>A. Nesje</name></json:item><json:item><name>M. Kvamme</name></json:item><json:item><name>N. Rye</name></json:item><json:item><name>R. Løvlie</name></json:item></author><host><volume>10</volume><pages><last>114</last><first>87</first></pages><author></author><title>Quaternary Science Review</title></host><title>Holocene glacier and climate history of the Jostedalsbreen region, western Norway; evidence from lake sediments and terrestrial deposits</title></json:item><json:item><author><json:item><name>A. Nesje</name></json:item><json:item><name>O. Lie</name></json:item><json:item><name>S.O. Dahl</name></json:item></author><host><volume>15</volume><pages><last>601</last><first>587</first></pages><author></author><title>Journal of Quaternary Science</title></host><title>Is the North Atlantic Oscillation reflected in Scandinavian glacier mass balance records</title></json:item><json:item><author><json:item><name>J. Oerlemans</name></json:item></author><host><pages><last>371</last><first>353</first></pages><author></author><title>Glacier Fluctuations and Climate Change</title></host><title>On the response of valley glaciers to climate change</title></json:item><json:item><author><json:item><name>J. Oerlemans</name></json:item></author><host><volume>264</volume><pages><last>245</last><first>243</first></pages><author></author><title>Science</title></host><title>Quantifying global warming from the retreat of glaciers</title></json:item><json:item><author><json:item><name>J. Oerlemans</name></json:item></author><host><volume>29</volume><pages><last>239</last><first>233</first></pages><author></author><title>Arctic and Alpine Research</title></host><title>Climate sensitivity of Franz Josef Glacier, New Zealand, as revealed by numerical modelling</title></json:item><json:item><author><json:item><name>A. Ohmura</name></json:item><json:item><name>P. Kasser</name></json:item><json:item><name>M. Funk</name></json:item></author><host><volume>38</volume><pages><last>411</last><first>397</first></pages><author></author><title>Journal of Glaciology</title></host><title>Climate at the equilibrium line of glaciers</title></json:item><json:item><author><json:item><name>G. Østrem</name></json:item><json:item><name>N. Haakensen</name></json:item><json:item><name>O. Melander</name></json:item></author><host><volume>22</volume><pages><first>315</first></pages><author></author><title>NVE Meddelelser Hydrologisk Avdeling</title></host><title>Atlas over breer i Nord‐Skandinavia</title></json:item><json:item><author><json:item><name>G. Østrem</name></json:item><json:item><name>K. Dale Selvig</name></json:item><json:item><name>K. Tandberg</name></json:item></author><host><volume>61</volume><pages><first>247</first></pages><author></author><title>NVE Meddelelser Hydrologisk Avdeling</title></host><title>Atlas over breer i Sør‐Norge</title></json:item><json:item><host><pages><first>380</first></pages><author></author><title>Paterson, W.S.B., 1994: The Physics of Glaciers, (third edition). Pergamon. Oxford . 380p.</title></host></json:item><json:item><author><json:item><name>V.A. Pohjola</name></json:item><json:item><name>J.C. Rogers</name></json:item></author><host><volume>47</volume><pages><last>36</last><first>29</first></pages><author></author><title>Quaternary Research</title></host><title>Atmospheric circulation and variations in Scandinavian glacier mass balance</title></json:item><json:item><author><json:item><name>S. C. Porter</name></json:item></author><host><volume>15</volume><pages><last>408</last><first>395</first></pages><author></author><title>Journal of Quaternary Science</title></host><title>Onset of Neoglaciation in the southern hemisphere</title></json:item><json:item><author><json:item><name>J.C. Rogers</name></json:item></author><host><volume>112</volume><pages><last>2015</last><first>1999</first></pages><author></author><title>Monthly Weather Review</title></host><title>The association between the North Atlantic Oscillation and the Southern Oscillation in the northern hemisphere</title></json:item><json:item><host><pages><first>416</first></pages><author></author><title>Röthlisberger, F., 1986: 10000 Jahre Gletschergeschichte der Erde. Sauerländer. Aarau . 416p.</title></host></json:item><json:item><author><json:item><name>M.J. Salinger</name></json:item></author><host><volume>25</volume><pages><last>86</last><first>77</first></pages><author></author><title>New Zealand Journal of Science</title></host><title>On the suggestion of post‐1950 wanning over New Zealand</title></json:item><json:item><author><json:item><name>M.J. Salinger</name></json:item><json:item><name>A.B. Mullan</name></json:item></author><host><volume>19</volume><pages><last>1071</last><first>1049</first></pages><author></author><title>International Journal of Climate</title></host><title>New Zealand climate: temperature and precipitation variations and their links with atmospheric circulation 1930–1994</title></json:item><json:item><author><json:item><name>M.J. Salinger</name></json:item><json:item><name>M.J. Heine</name></json:item><json:item><name>C.J. Burrows</name></json:item></author><host><volume>26</volume><pages><last>338</last><first>321</first></pages><author></author><title>New Zealand Journal of Science</title></host><title>Variations of Stocking (Te Wae Wae) Glacier, Mount Cook, and climate relationships</title></json:item><json:item><author><json:item><name>M.J. Salinger</name></json:item><json:item><name>J.A. Renwick</name></json:item><json:item><name>A.B. Mullan</name></json:item></author><host><volume>21</volume><pages><last>1721</last><first>1705</first></pages><author></author><title>International Journal of Climate</title></host><title>Interdecadal Pacific Oscillation and South Pacific climate</title></json:item><json:item><host><pages><last>200</last><first>195</first></pages><author></author><title>Soons, J. M., 1971: Recent changes in the Franz Josef Glacier. Proceedings, Sixth New Zealand Geography Conference. Christchurch . 195–200.</title></host></json:item><json:item><author><json:item><name>R.P. Suggate</name></json:item></author><host><volume>1</volume><pages><last>429</last><first>422</first></pages><author></author><title>Journal of Glaciology</title></host><title>Franz Josef and other glaciers of the Southern Alps, New Zealand</title></json:item><json:item><author><json:item><name>A.M. Tvede</name></json:item><json:item><name>O. Liestøl</name></json:item></author><host><volume>1976</volume><pages><last>234</last><first>225</first></pages><author></author><title>Norsk Polarin-stitutt Årbok</title></host><title>Blomsterskardbreen, Folge‐fonni, mass balance and recent fluctuations</title></json:item><json:item><author><json:item><name>P. Wardle</name></json:item></author><host><volume>11</volume><pages><last>388</last><first>349</first></pages><author></author><title>New Zealand Journal of Botany</title></host><title>Variations of the glaciers of Westland National Park and the Hooker Range, New Zealand</title></json:item><json:item><author><json:item><name>S. Winkler</name></json:item></author><host><volume>431</volume><pages><last>47</last><first>33</first></pages><author></author><title>Norges Geologiske Undersøkelse Bulletin</title></host><title>Front variations of outlet glaciers from Jostedalsbreen, western Norway, during the twentieth century</title></json:item><json:item><host><author></author><title>Winkler, S., 2001: Untersuchungen zur Klima‐ und Morphodynamik in skandinavischen Gebirgsregionen während des Holozän‐ein Vergleich ihrer Wechselwirkungen und Pro‐zeβsysteme im überregionalen Kontext kaltgemäβigter maritimer Gebirgsregionen. Unpublished ‘Habilitationsschrift’. University of Trier.</title></host></json:item><json:item><author><json:item><name>S. Winkler</name></json:item></author><host><volume>13</volume><pages><last>95</last><first>83</first></pages><author></author><title>The Holocene</title></host><title>A new interpretation of the date of the ‘Little Ice Age’ maximum at Svartisen and Okstindan, northern Norway</title></json:item><json:item><author><json:item><name>S. Winkler</name></json:item></author><host><volume>14</volume><issue>6</issue><author></author><title>The Holocene</title></host><title>Lichenometric dating of the ‘Little Ice Age’ maximum in Mt Cook National Park, Southern Alps, New Zealand</title></json:item><json:item><author><json:item><name>S. Winkler</name></json:item></author><host><pages><first>48</first></pages><author></author><title>New Zealand Journal of Geology and Geophysics</title></host><title>The ‘Schmidt hammer’ as a relative‐age dating technique: potential and limitations of its application on Holocene moraines in Mt Cook National Park, Southern Alps, New Zealand</title></json:item><json:item><author><json:item><name>S. Winkler</name></json:item><json:item><name>N. Haakensen</name></json:item></author><host><volume>143</volume><pages><last>304</last><first>291</first></pages><author></author><title>Petermanns Geographische Mitteilungen</title></host><title>Kritische Überprüfung der Möglichkeit zur Prognose des Gletscherverhaltens auf Grundlage von Modellierungen – dargestellt anhand von regionalen Beispielen aus Norwegen</title></json:item><json:item><author><json:item><name>S. Winkler</name></json:item><json:item><name>N. Haakensen</name></json:item><json:item><name>A. Nesje</name></json:item><json:item><name>N. Rye</name></json:item></author><host><volume>141</volume><pages><last>63</last><first>43</first></pages><author></author><title>Petermanns Geographische Mitteilungen</title></host><title>Glaziale Dynamik in Westnorwegen – Ablauf und Ursachen des aktuellen Gletschervorstoβes am Jostedalsbreen</title></json:item></refBibs><genre><json:string>article</json:string></genre><host><volume>87</volume><publisherId><json:string>GEOA</json:string></publisherId><pages><total>17</total><last>157</last><first>141</first></pages><issn><json:string>0435-3676</json:string></issn><issue>1</issue><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1468-0459</json:string></eissn><title>Geografiska Annaler: Series A, Physical Geography</title><doi><json:string>10.1111/(ISSN)1468-0459</json:string></doi></host><categories><wos><json:string>science</json:string><json:string>geology</json:string><json:string>geography, physical</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>earth & environmental sciences</json:string><json:string>paleontology</json:string></scienceMetrix></categories><publicationDate>2005</publicationDate><copyrightDate>2005</copyrightDate><doi><json:string>10.1111/j.0435-3676.2005.00249.x</json:string></doi><id>854CD15ED50A44B84B705B93B1D01BB74A0BA51D</id><score>0.022456028</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/854CD15ED50A44B84B705B93B1D01BB74A0BA51D/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/854CD15ED50A44B84B705B93B1D01BB74A0BA51D/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/854CD15ED50A44B84B705B93B1D01BB74A0BA51D/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><availability><p>WILEY</p></availability><date>2005</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES</title><author xml:id="author-1"><persName><forename type="first">T.</forename><surname>CHINN</surname></persName><affiliation>Lake Hawea, Wanaka, Otago, New Zealand</affiliation><affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</affiliation></author><author xml:id="author-2"><persName><forename type="first">S.</forename><surname>WINKLER</surname></persName><affiliation>Department of Geography, University of Würzburg, Würzburg, Germany</affiliation><affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</affiliation></author><author xml:id="author-3"><persName><forename type="first">M.J.</forename><surname>SALINGER</surname></persName><affiliation>National Institute of Water and Atmospheric Research, Auckland, New Zealand</affiliation><affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</affiliation></author><author xml:id="author-4"><persName><forename type="first">N.</forename><surname>HAAKENSEN</surname></persName><affiliation>Norwegian Water Resources and Energy Directorate (NVE), Oslo, Norway</affiliation><affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</affiliation></author></analytic><monogr><title level="j">Geografiska Annaler: Series A, Physical Geography</title><idno type="pISSN">0435-3676</idno><idno type="eISSN">1468-0459</idno><idno type="DOI">10.1111/(ISSN)1468-0459</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><pubPlace>Oxford, UK</pubPlace><date type="published" when="2005-03"></date><biblScope unit="volume">87</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="141">141</biblScope><biblScope unit="page" to="157">157</biblScope></imprint></monogr><idno type="istex">854CD15ED50A44B84B705B93B1D01BB74A0BA51D</idno><idno type="DOI">10.1111/j.0435-3676.2005.00249.x</idno><idno type="ArticleID">GEOA249</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>2005</date></creation><langUsage><language ident="en">en</language></langUsage><abstract><p>ABSTRACT. Norway and New Zealand both experienced recent glacial advances, commencing in the early 1980s and ceasing around 2000, which were more extensive than any other since the end of the Little Ice Age. Common to both countries, the positive glacier balances are associated with an increase in the strength of westerly atmospheric circulation which brought increased precipitation. In Norway, the changes are also associated with lower ablation season temperatures. In New Zealand, where the positive balances were distributed uniformly throughout the Southern Alps, the period of increased mass balance was coincident with a change in the Interdecadal Pacific Oscillation and an associated increase in El Niño/Southern Oscillation events. In Norway, the positive balances occurred across a strong west‐east gradient with no balance increases to the continental glaciers of Scandinavia. The Norwegian advances are linked to strongly positive North Atlantic Oscillation events which caused an overall increase of precipitation in the winter accumulation season and a general shift of maximum precipitation from autumn towards winter. These cases both show the influence of atmospheric circulation on maritime glaciers.</p></abstract><textClass xml:lang="en"><keywords scheme="keyword"><list><head>keywords</head><item><term>glaciers</term></item><item><term>mass balance</term></item><item><term>advance</term></item><item><term>NAO</term></item><item><term>IPO</term></item><item><term>ENSO/SOI</term></item><item><term>Norway</term></item><item><term>New Zealand</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="2005-03">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/854CD15ED50A44B84B705B93B1D01BB74A0BA51D/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component version="2.0" type="serialArticle" xml:lang="en"><header><publicationMeta level="product"><publisherInfo><publisherName>Blackwell Publishing Ltd</publisherName><publisherLoc>Oxford, UK</publisherLoc></publisherInfo><doi origin="wiley" registered="yes">10.1111/(ISSN)1468-0459</doi><issn type="print">0435-3676</issn><issn type="electronic">1468-0459</issn><idGroup><id type="product" value="GEOA"></id><id type="publisherDivision" value="ST"></id></idGroup><titleGroup><title type="main" sort="GEOGRAFISKA ANNALER SERIES A PHYSICAL GEOGRAPHY">Geografiska Annaler: Series A, Physical Geography</title></titleGroup></publicationMeta><publicationMeta level="part" position="03001"><doi origin="wiley">10.1111/geoa.2005.87.issue-1</doi><numberingGroup><numbering type="journalVolume" number="87">87</numbering><numbering type="journalIssue" number="1">1</numbering></numberingGroup><coverDate startDate="2005-03">March 2005</coverDate></publicationMeta><publicationMeta level="unit" type="article" position="10" status="forIssue"><doi origin="wiley">10.1111/j.0435-3676.2005.00249.x</doi><idGroup><id type="unit" value="GEOA249"></id></idGroup><countGroup><count type="pageTotal" number="17"></count></countGroup><eventGroup><event type="firstOnline" date="2005-07-22"></event><event type="publishedOnlineFinalForm" date="2005-07-22"></event><event type="xmlConverted" agent="Converter:BPG_TO_WML3G version:2.3.5 mode:FullText source:HeaderRef result:HeaderRef" date="2010-04-07"></event><event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:3.8.8" date="2014-01-26"></event><event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-10-16"></event></eventGroup><numberingGroup><numbering type="pageFirst" number="141">141</numbering><numbering type="pageLast" number="157">157</numbering></numberingGroup><correspondenceTo><lineatedText><line>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.</line><line>S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, Germany</line><line>M.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New Zealand</line><line>N. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</line></lineatedText></correspondenceTo><linkGroup><link type="toTypesetVersion" href="file:GEOA.GEOA249.pdf"></link></linkGroup></publicationMeta><contentMeta><unparsedEditorialHistory>Manuscript received August 2004, revised and accepted December 2004</unparsedEditorialHistory><countGroup><count type="referenceTotal" number="80"></count><count type="linksCrossRef" number="8"></count></countGroup><titleGroup><title type="main">RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES</title></titleGroup><creators><creator creatorRole="author" xml:id="cr1" affiliationRef="#a1" corresponding="yes"><personName><givenNames>T.</givenNames><familyName>CHINN</familyName></personName></creator><creator creatorRole="author" xml:id="cr2" affiliationRef="#a2" corresponding="yes"><personName><givenNames>S.</givenNames><familyName>WINKLER</familyName></personName></creator><creator creatorRole="author" xml:id="cr3" affiliationRef="#a3" corresponding="yes"><personName><givenNames>M.J.</givenNames><familyName>SALINGER</familyName></personName></creator><creator creatorRole="author" xml:id="cr4" affiliationRef="#a4" corresponding="yes"><personName><givenNames>N.</givenNames><familyName>HAAKENSEN</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="a1" countryCode="NZ"><unparsedAffiliation>Lake Hawea, Wanaka, Otago, New Zealand</unparsedAffiliation></affiliation><affiliation xml:id="a2" countryCode="DE"><unparsedAffiliation>
Department of Geography, University of Würzburg, Würzburg, Germany</unparsedAffiliation></affiliation><affiliation xml:id="a3" countryCode="NZ"><unparsedAffiliation>
National Institute of Water and Atmospheric Research, Auckland, New Zealand</unparsedAffiliation></affiliation><affiliation xml:id="a4" countryCode="NO"><unparsedAffiliation>
Norwegian Water Resources and Energy Directorate (NVE), Oslo, Norway</unparsedAffiliation></affiliation></affiliationGroup><keywordGroup xml:lang="en"><keyword xml:id="k1">glaciers</keyword><keyword xml:id="k2">mass balance</keyword><keyword xml:id="k3">advance</keyword><keyword xml:id="k4">NAO</keyword><keyword xml:id="k5">IPO</keyword><keyword xml:id="k6">ENSO/SOI</keyword><keyword xml:id="k7">Norway</keyword><keyword xml:id="k8">New Zealand</keyword></keywordGroup><abstractGroup><abstract type="main" xml:lang="en"><p><b>ABSTRACT. </b> Norway and New Zealand both experienced recent glacial advances, commencing in the early 1980s and ceasing around 2000, which were more extensive than any other since the end of the Little Ice Age. Common to both countries, the positive glacier balances are associated with an increase in the strength of westerly atmospheric circulation which brought increased precipitation. In Norway, the changes are also associated with lower ablation season temperatures. In New Zealand, where the positive balances were distributed uniformly throughout the Southern Alps, the period of increased mass balance was coincident with a change in the Interdecadal Pacific Oscillation and an associated increase in El Niño/Southern Oscillation events. In Norway, the positive balances occurred across a strong west‐east gradient with no balance increases to the continental glaciers of Scandinavia. The Norwegian advances are linked to strongly positive North Atlantic Oscillation events which caused an overall increase of precipitation in the winter accumulation season and a general shift of maximum precipitation from autumn towards winter. These cases both show the influence of atmospheric circulation on maritime glaciers.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES</title></titleInfo><name type="personal"><namePart type="given">T.</namePart><namePart type="family">CHINN</namePart><affiliation>Lake Hawea, Wanaka, Otago, New Zealand</affiliation><affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">S.</namePart><namePart type="family">WINKLER</namePart><affiliation>Department of Geography, University of Würzburg, Würzburg, Germany</affiliation><affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">M.J.</namePart><namePart type="family">SALINGER</namePart><affiliation>National Institute of Water and Atmospheric Research, Auckland, New Zealand</affiliation><affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">N.</namePart><namePart type="family">HAAKENSEN</namePart><affiliation>Norwegian Water Resources and Energy Directorate (NVE), Oslo, Norway</affiliation><affiliation>T. Chinn, 20 Muir Road, Lake Hawea, RD2 Wana‐ka, Otago, New Zealand.S. Winkler, Department of Geography, University of Wurzburg, 97074, Würzburg, GermanyM.J. Salinger, national institute of water and athmospheric Research, Box 109–695, Auckland, New ZealandN. Haakensen, Norwegian Water Resources and Energy Directorate (NVE), PB. 5091 Majorstua, N‐0301 Oslo, Norway</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><place><placeTerm type="text">Oxford, UK</placeTerm></place><dateIssued encoding="w3cdtf">2005-03</dateIssued><edition>Manuscript received August 2004, revised and accepted December 2004</edition><copyrightDate encoding="w3cdtf">2005</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="references">80</extent></physicalDescription><abstract>ABSTRACT. Norway and New Zealand both experienced recent glacial advances, commencing in the early 1980s and ceasing around 2000, which were more extensive than any other since the end of the Little Ice Age. Common to both countries, the positive glacier balances are associated with an increase in the strength of westerly atmospheric circulation which brought increased precipitation. In Norway, the changes are also associated with lower ablation season temperatures. In New Zealand, where the positive balances were distributed uniformly throughout the Southern Alps, the period of increased mass balance was coincident with a change in the Interdecadal Pacific Oscillation and an associated increase in El Niño/Southern Oscillation events. In Norway, the positive balances occurred across a strong west‐east gradient with no balance increases to the continental glaciers of Scandinavia. The Norwegian advances are linked to strongly positive North Atlantic Oscillation events which caused an overall increase of precipitation in the winter accumulation season and a general shift of maximum precipitation from autumn towards winter. These cases both show the influence of atmospheric circulation on maritime glaciers.</abstract><subject lang="en"><genre>keywords</genre><topic>glaciers</topic><topic>mass balance</topic><topic>advance</topic><topic>NAO</topic><topic>IPO</topic><topic>ENSO/SOI</topic><topic>Norway</topic><topic>New Zealand</topic></subject><relatedItem type="host"><titleInfo><title>Geografiska Annaler: Series A, Physical Geography</title></titleInfo><genre type="journal">journal</genre><identifier type="ISSN">0435-3676</identifier><identifier type="eISSN">1468-0459</identifier><identifier type="DOI">10.1111/(ISSN)1468-0459</identifier><identifier type="PublisherID">GEOA</identifier><part><date>2005</date><detail type="volume"><caption>vol.</caption><number>87</number></detail><detail type="issue"><caption>no.</caption><number>1</number></detail><extent unit="pages"><start>141</start><end>157</end><total>17</total></extent></part></relatedItem><identifier type="istex">854CD15ED50A44B84B705B93B1D01BB74A0BA51D</identifier><identifier type="DOI">10.1111/j.0435-3676.2005.00249.x</identifier><identifier type="ArticleID">GEOA249</identifier><recordInfo><recordContentSource>WILEY</recordContentSource><recordOrigin>Blackwell Publishing Ltd</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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