Current Ice Loss in Small Glacier Systems of the Arctic Islands (Iceland, Svalbard, and the Russian High Arctic) from Satellite Gravimetry

Recent climate changes have brought about significant ice sheets and glacier melting in many parts of the world. Satellite gravimetry by the Gravity Recovery and Climate Experiment (GRACE) revealed that such ice melting also occurs in small glacier systems in the Arctic region, i.e., Iceland, Svalba...

Full description

Bibliographic Details
Main Authors: Matsuo, Koji, Heki, Kosuke
Format: Article in Journal/Newspaper
Language:English
Published: Terrestrial Atmospheric and Oceanic Sciences (TAO)
Subjects:
453
Online Access:http://hdl.handle.net/2115/53027
https://doi.org/10.3319/TAO.2013.02.22.01(TibXS
id fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/53027
record_format openpolar
spelling fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/53027 2023-05-15T14:34:28+02:00 Current Ice Loss in Small Glacier Systems of the Arctic Islands (Iceland, Svalbard, and the Russian High Arctic) from Satellite Gravimetry Matsuo, Koji Heki, Kosuke http://hdl.handle.net/2115/53027 https://doi.org/10.3319/TAO.2013.02.22.01(TibXS eng eng Terrestrial Atmospheric and Oceanic Sciences (TAO) http://tao.cgu.org.tw http://hdl.handle.net/2115/53027 Terrestrial, Atmospheric and Oceanic Sciences, 24(4-1): 657-670 http://dx.doi.org/10.3319/TAO.2013.02.22.01(TibXS) Glacier Gravity GRACE The Arctic Islands Ice loss 453 article fthokunivhus https://doi.org/10.3319/TAO.2013.02.22.01(TibXS 2022-11-18T01:02:52Z Recent climate changes have brought about significant ice sheets and glacier melting in many parts of the world. Satellite gravimetry by the Gravity Recovery and Climate Experiment (GRACE) revealed that such ice melting also occurs in small glacier systems in the Arctic region, i.e., Iceland, Svalbard, and the Russian High Arctic. Using monthly gravity solutions from GRACE during 2004.02 - 2012.01, we obtained the average ice loss rates of 10.9 ± 2.1, 3.6 ± 2.9, and 6.9 ± 7.4 Gt yr-1, for these three glacial systems, respectively. The total ice loss rate is 21.4 ± 12.4 Gt yr-1, about twice as fast as the average rate over a ~40 years interval before the studied period. We found that the ice loss rates in Svalbard and Novaya Zemlya, in the Russian High Arctic, had significant temporal variability, showing decreasing trend before 2008 and increasing trend around the winter of 2009/2010, respectively. Due to such variability, the total ice loss rate becomes as high as 32.9 ± 19.2 Gt yr-1 during 2004.02 - 2008.01. Such variability in the rate might reflect the strong negative Arctic Oscillation (AO) in the northern hemisphere winter of 2009/2010. Article in Journal/Newspaper Arctic glacier glacier Iceland Novaya Zemlya Svalbard Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Arctic Svalbard
institution Open Polar
collection Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP)
op_collection_id fthokunivhus
language English
topic Glacier
Gravity
GRACE
The Arctic Islands
Ice loss
453
spellingShingle Glacier
Gravity
GRACE
The Arctic Islands
Ice loss
453
Matsuo, Koji
Heki, Kosuke
Current Ice Loss in Small Glacier Systems of the Arctic Islands (Iceland, Svalbard, and the Russian High Arctic) from Satellite Gravimetry
topic_facet Glacier
Gravity
GRACE
The Arctic Islands
Ice loss
453
description Recent climate changes have brought about significant ice sheets and glacier melting in many parts of the world. Satellite gravimetry by the Gravity Recovery and Climate Experiment (GRACE) revealed that such ice melting also occurs in small glacier systems in the Arctic region, i.e., Iceland, Svalbard, and the Russian High Arctic. Using monthly gravity solutions from GRACE during 2004.02 - 2012.01, we obtained the average ice loss rates of 10.9 ± 2.1, 3.6 ± 2.9, and 6.9 ± 7.4 Gt yr-1, for these three glacial systems, respectively. The total ice loss rate is 21.4 ± 12.4 Gt yr-1, about twice as fast as the average rate over a ~40 years interval before the studied period. We found that the ice loss rates in Svalbard and Novaya Zemlya, in the Russian High Arctic, had significant temporal variability, showing decreasing trend before 2008 and increasing trend around the winter of 2009/2010, respectively. Due to such variability, the total ice loss rate becomes as high as 32.9 ± 19.2 Gt yr-1 during 2004.02 - 2008.01. Such variability in the rate might reflect the strong negative Arctic Oscillation (AO) in the northern hemisphere winter of 2009/2010.
format Article in Journal/Newspaper
author Matsuo, Koji
Heki, Kosuke
author_facet Matsuo, Koji
Heki, Kosuke
author_sort Matsuo, Koji
title Current Ice Loss in Small Glacier Systems of the Arctic Islands (Iceland, Svalbard, and the Russian High Arctic) from Satellite Gravimetry
title_short Current Ice Loss in Small Glacier Systems of the Arctic Islands (Iceland, Svalbard, and the Russian High Arctic) from Satellite Gravimetry
title_full Current Ice Loss in Small Glacier Systems of the Arctic Islands (Iceland, Svalbard, and the Russian High Arctic) from Satellite Gravimetry
title_fullStr Current Ice Loss in Small Glacier Systems of the Arctic Islands (Iceland, Svalbard, and the Russian High Arctic) from Satellite Gravimetry
title_full_unstemmed Current Ice Loss in Small Glacier Systems of the Arctic Islands (Iceland, Svalbard, and the Russian High Arctic) from Satellite Gravimetry
title_sort current ice loss in small glacier systems of the arctic islands (iceland, svalbard, and the russian high arctic) from satellite gravimetry
publisher Terrestrial Atmospheric and Oceanic Sciences (TAO)
url http://hdl.handle.net/2115/53027
https://doi.org/10.3319/TAO.2013.02.22.01(TibXS
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
glacier
glacier
Iceland
Novaya Zemlya
Svalbard
genre_facet Arctic
glacier
glacier
Iceland
Novaya Zemlya
Svalbard
op_relation http://tao.cgu.org.tw
http://hdl.handle.net/2115/53027
Terrestrial, Atmospheric and Oceanic Sciences, 24(4-1): 657-670
http://dx.doi.org/10.3319/TAO.2013.02.22.01(TibXS)
op_doi https://doi.org/10.3319/TAO.2013.02.22.01(TibXS
_version_ 1766307493892325376