Glacier mass balance measurements on Fourcade and Polar Club glacier, King George Island
The east coast of the AP is highly influenced by cold and dry air masses stemming from the adjacent Weddell Sea. By the contrary, the west coast jointly with the South Shetland Islands are directly exposed to the humid and relatively warm air masses from the South Pacific Ocean carried by the strong...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.854454 2023-05-15T14:03:05+02:00 Glacier mass balance measurements on Fourcade and Polar Club glacier, King George Island Falk, Ulrike López, Damián Sala, Hernán LATITUDE: -62.236060 * LONGITUDE: -58.613530 * DATE/TIME START: 2010-12-05T00:00:00 * DATE/TIME END: 2015-06-17T00:00:00 * MINIMUM ELEVATION: 230.0 m * MAXIMUM ELEVATION: 230.0 m 2015-10-29 text/tab-separated-values, 186 data points https://doi.pangaea.de/10.1594/PANGAEA.854454 https://doi.org/10.1594/PANGAEA.854454 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.854454 https://doi.org/10.1594/PANGAEA.854454 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Falk, Ulrike; López, Damián; Sala, Hernán (in prep.): Tipping point of glacier mass balance changes for the inland ice cap of King George Island, West Antarctica. Automatic weather station AWS Calculated DATE/TIME IMCOAST/IMCONet Impact of climate induced glacier melt on marine coastal systems Antarctica King George Island Antarctic Peninsula Length difference Melt rate in water equivalent per day Warszawa_Icefield_AWS Dataset 2015 ftpangaea https://doi.org/10.1594/PANGAEA.854454 2023-01-20T09:06:26Z The east coast of the AP is highly influenced by cold and dry air masses stemming from the adjacent Weddell Sea. By the contrary, the west coast jointly with the South Shetland Islands are directly exposed to the humid and relatively warm air masses from the South Pacific Ocean carried by the strong and persistent westerly winds. Systematic glaciological field studies are very scarce on both sides of the AP, among them can be mentioned a mass-balance program performed continuously since summer 1998/99 by the Instituto Antártico Argentino (IAA) on Vega Island, James Ross Archipelago, on the northeastern flank of the AP. Another continuous plurianual glaciological research has been initiated in 2010 jointly by the University of Bonn and the IAA at the Fourcade Glacier on King George Island (KGI) within the framework of the ESF project IMCOAST (FK 03F0617B). Two transects of mass balance stakes were installed from the top of the Warszawa Ice Dome down to the border of the glaciers Fourcade and Polar Club, to serve for calibration and validation of modeling efforts. The stakes were measured at the beginning and end of each summer field campaign in November 2010, February - March 2011, January - March 2012, and especially during the austral winter 2012 up to March 2013 every 10 to 14 days depending on weather conditions. During the austral winter 2013 and until June 2014 the measurements were conducted every 20 to 30 days, weather permitting. Snow density was measured as well in every field trip from June 2012 until June 2104, establishing a rather homogeneous value along the different parts of the glacier. Snow density in late summer, rho_s is usually higher than the one in late winter, rho_w. Seasonal average values were calculated for the area covered by the mass balance stakes, being rho_s= 471 Kg/m**3 and rho_w = 363 Kg/m**3. Dataset Antarc* Antarctic Antarctic Peninsula Antarctica Instituto Antártico Argentino King George Island Ross Archipelago South Shetland Islands Vega Island Weddell Sea PANGAEA - Data Publisher for Earth & Environmental Science Antarctic Antarctic Peninsula Argentino Austral Fourcade ENVELOPE(-62.490,-62.490,-64.612,-64.612) Fourcade Glacier ENVELOPE(-58.666,-58.666,-62.216,-62.216) King George Island Pacific Polar Club Glacier ENVELOPE(-58.533,-58.533,-62.233,-62.233) Ross Archipelago ENVELOPE(167.000,167.000,-77.500,-77.500) South Shetland Islands Vega Island ENVELOPE(-57.500,-57.500,-63.833,-63.833) Weddell Weddell Sea ENVELOPE(-58.613530,-58.613530,-62.236060,-62.236060) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Automatic weather station AWS Calculated DATE/TIME IMCOAST/IMCONet Impact of climate induced glacier melt on marine coastal systems Antarctica King George Island Antarctic Peninsula Length difference Melt rate in water equivalent per day Warszawa_Icefield_AWS |
spellingShingle |
Automatic weather station AWS Calculated DATE/TIME IMCOAST/IMCONet Impact of climate induced glacier melt on marine coastal systems Antarctica King George Island Antarctic Peninsula Length difference Melt rate in water equivalent per day Warszawa_Icefield_AWS Falk, Ulrike López, Damián Sala, Hernán Glacier mass balance measurements on Fourcade and Polar Club glacier, King George Island |
topic_facet |
Automatic weather station AWS Calculated DATE/TIME IMCOAST/IMCONet Impact of climate induced glacier melt on marine coastal systems Antarctica King George Island Antarctic Peninsula Length difference Melt rate in water equivalent per day Warszawa_Icefield_AWS |
description |
The east coast of the AP is highly influenced by cold and dry air masses stemming from the adjacent Weddell Sea. By the contrary, the west coast jointly with the South Shetland Islands are directly exposed to the humid and relatively warm air masses from the South Pacific Ocean carried by the strong and persistent westerly winds. Systematic glaciological field studies are very scarce on both sides of the AP, among them can be mentioned a mass-balance program performed continuously since summer 1998/99 by the Instituto Antártico Argentino (IAA) on Vega Island, James Ross Archipelago, on the northeastern flank of the AP. Another continuous plurianual glaciological research has been initiated in 2010 jointly by the University of Bonn and the IAA at the Fourcade Glacier on King George Island (KGI) within the framework of the ESF project IMCOAST (FK 03F0617B). Two transects of mass balance stakes were installed from the top of the Warszawa Ice Dome down to the border of the glaciers Fourcade and Polar Club, to serve for calibration and validation of modeling efforts. The stakes were measured at the beginning and end of each summer field campaign in November 2010, February - March 2011, January - March 2012, and especially during the austral winter 2012 up to March 2013 every 10 to 14 days depending on weather conditions. During the austral winter 2013 and until June 2014 the measurements were conducted every 20 to 30 days, weather permitting. Snow density was measured as well in every field trip from June 2012 until June 2104, establishing a rather homogeneous value along the different parts of the glacier. Snow density in late summer, rho_s is usually higher than the one in late winter, rho_w. Seasonal average values were calculated for the area covered by the mass balance stakes, being rho_s= 471 Kg/m**3 and rho_w = 363 Kg/m**3. |
format |
Dataset |
author |
Falk, Ulrike López, Damián Sala, Hernán |
author_facet |
Falk, Ulrike López, Damián Sala, Hernán |
author_sort |
Falk, Ulrike |
title |
Glacier mass balance measurements on Fourcade and Polar Club glacier, King George Island |
title_short |
Glacier mass balance measurements on Fourcade and Polar Club glacier, King George Island |
title_full |
Glacier mass balance measurements on Fourcade and Polar Club glacier, King George Island |
title_fullStr |
Glacier mass balance measurements on Fourcade and Polar Club glacier, King George Island |
title_full_unstemmed |
Glacier mass balance measurements on Fourcade and Polar Club glacier, King George Island |
title_sort |
glacier mass balance measurements on fourcade and polar club glacier, king george island |
publisher |
PANGAEA |
publishDate |
2015 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.854454 https://doi.org/10.1594/PANGAEA.854454 |
op_coverage |
LATITUDE: -62.236060 * LONGITUDE: -58.613530 * DATE/TIME START: 2010-12-05T00:00:00 * DATE/TIME END: 2015-06-17T00:00:00 * MINIMUM ELEVATION: 230.0 m * MAXIMUM ELEVATION: 230.0 m |
long_lat |
ENVELOPE(-62.490,-62.490,-64.612,-64.612) ENVELOPE(-58.666,-58.666,-62.216,-62.216) ENVELOPE(-58.533,-58.533,-62.233,-62.233) ENVELOPE(167.000,167.000,-77.500,-77.500) ENVELOPE(-57.500,-57.500,-63.833,-63.833) ENVELOPE(-58.613530,-58.613530,-62.236060,-62.236060) |
geographic |
Antarctic Antarctic Peninsula Argentino Austral Fourcade Fourcade Glacier King George Island Pacific Polar Club Glacier Ross Archipelago South Shetland Islands Vega Island Weddell Weddell Sea |
geographic_facet |
Antarctic Antarctic Peninsula Argentino Austral Fourcade Fourcade Glacier King George Island Pacific Polar Club Glacier Ross Archipelago South Shetland Islands Vega Island Weddell Weddell Sea |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctica Instituto Antártico Argentino King George Island Ross Archipelago South Shetland Islands Vega Island Weddell Sea |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctica Instituto Antártico Argentino King George Island Ross Archipelago South Shetland Islands Vega Island Weddell Sea |
op_source |
Supplement to: Falk, Ulrike; López, Damián; Sala, Hernán (in prep.): Tipping point of glacier mass balance changes for the inland ice cap of King George Island, West Antarctica. |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.854454 https://doi.org/10.1594/PANGAEA.854454 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.854454 |
_version_ |
1766273591518691328 |