RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES BY
ison of their glaciological and meteorological causes. Geogr. Ann., 87 A (1): 141–157. ABSTRACT. Norway and New Zealand both experi-enced 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. Comm...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.510.2921 2023-05-15T16:21:55+02:00 RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES BY Geografiska Annaler A T. Chinn S. Winkler M. J. Salinger N. Haakensen The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.510.2921 http://meteo.lcd.lu/globalwarming/Winkler/Chinnetal-1.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.510.2921 http://meteo.lcd.lu/globalwarming/Winkler/Chinnetal-1.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://meteo.lcd.lu/globalwarming/Winkler/Chinnetal-1.pdf Key words glaciers mass balance advance NAO IPO ENSO/ SOI text ftciteseerx 2016-01-08T09:36:51Z ison of their glaciological and meteorological causes. Geogr. Ann., 87 A (1): 141–157. ABSTRACT. Norway and New Zealand both experi-enced 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 posi-tive 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 in-creased mass balance was coincident with a change in the Interdecadal Pacific Oscillation and an asso-ciated 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 pos-itive North Atlantic Oscillation events which caused an overall increase of precipitation in the winter ac-cumulation season and a general shift of maximum precipitation from autumn towards winter. These cases both show the influence of atmospheric circu-lation on maritime glaciers. Text glacier North Atlantic North Atlantic oscillation Unknown New Zealand Norway Pacific Posi ENVELOPE(24.179,24.179,65.691,65.691) Soi ENVELOPE(30.704,30.704,66.481,66.481) Tive ENVELOPE(12.480,12.480,65.107,65.107) |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
topic |
Key words glaciers mass balance advance NAO IPO ENSO/ SOI |
spellingShingle |
Key words glaciers mass balance advance NAO IPO ENSO/ SOI Geografiska Annaler A T. Chinn S. Winkler M. J. Salinger N. Haakensen RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES BY |
topic_facet |
Key words glaciers mass balance advance NAO IPO ENSO/ SOI |
description |
ison of their glaciological and meteorological causes. Geogr. Ann., 87 A (1): 141–157. ABSTRACT. Norway and New Zealand both experi-enced 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 posi-tive 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 in-creased mass balance was coincident with a change in the Interdecadal Pacific Oscillation and an asso-ciated 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 pos-itive North Atlantic Oscillation events which caused an overall increase of precipitation in the winter ac-cumulation season and a general shift of maximum precipitation from autumn towards winter. These cases both show the influence of atmospheric circu-lation on maritime glaciers. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Geografiska Annaler A T. Chinn S. Winkler M. J. Salinger N. Haakensen |
author_facet |
Geografiska Annaler A T. Chinn S. Winkler M. J. Salinger N. Haakensen |
author_sort |
Geografiska Annaler A |
title |
RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES BY |
title_short |
RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES BY |
title_full |
RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES BY |
title_fullStr |
RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES BY |
title_full_unstemmed |
RECENT GLACIER ADVANCES IN NORWAY AND NEW ZEALAND: A COMPARISON OF THEIR GLACIOLOGICAL AND METEOROLOGICAL CAUSES BY |
title_sort |
recent glacier advances in norway and new zealand: a comparison of their glaciological and meteorological causes by |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.510.2921 http://meteo.lcd.lu/globalwarming/Winkler/Chinnetal-1.pdf |
long_lat |
ENVELOPE(24.179,24.179,65.691,65.691) ENVELOPE(30.704,30.704,66.481,66.481) ENVELOPE(12.480,12.480,65.107,65.107) |
geographic |
New Zealand Norway Pacific Posi Soi Tive |
geographic_facet |
New Zealand Norway Pacific Posi Soi Tive |
genre |
glacier North Atlantic North Atlantic oscillation |
genre_facet |
glacier North Atlantic North Atlantic oscillation |
op_source |
http://meteo.lcd.lu/globalwarming/Winkler/Chinnetal-1.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.510.2921 http://meteo.lcd.lu/globalwarming/Winkler/Chinnetal-1.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766009890162081792 |