Brief communication: Increased glacier mass loss in the Russian High Arctic (2010–2017)

Glaciers in the Russian High Arctic have been subject to extensive atmospheric warming due to global climate change, yet their contribution to sea level rise has been relatively small over the past decades. Here we show surface elevation change measurements and geodetic mass balances of 93 % of all...

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Published in:The Cryosphere
Main Authors: C. Sommer, T. Seehaus, A. Glazovsky, M. H. Braun
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-16-35-2022
https://doaj.org/article/5da1b74c26914c94aa11929261ae0dbe
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spelling ftdoajarticles:oai:doaj.org/article:5da1b74c26914c94aa11929261ae0dbe 2023-05-15T14:57:16+02:00 Brief communication: Increased glacier mass loss in the Russian High Arctic (2010–2017) C. Sommer T. Seehaus A. Glazovsky M. H. Braun 2022-01-01T00:00:00Z https://doi.org/10.5194/tc-16-35-2022 https://doaj.org/article/5da1b74c26914c94aa11929261ae0dbe EN eng Copernicus Publications https://tc.copernicus.org/articles/16/35/2022/tc-16-35-2022.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-16-35-2022 1994-0416 1994-0424 https://doaj.org/article/5da1b74c26914c94aa11929261ae0dbe The Cryosphere, Vol 16, Pp 35-42 (2022) Environmental sciences GE1-350 Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.5194/tc-16-35-2022 2022-12-31T15:14:09Z Glaciers in the Russian High Arctic have been subject to extensive atmospheric warming due to global climate change, yet their contribution to sea level rise has been relatively small over the past decades. Here we show surface elevation change measurements and geodetic mass balances of 93 % of all glacierized areas of Novaya Zemlya, Severnaya Zemlya, and Franz Josef Land using interferometric synthetic aperture radar measurements taken between 2010 and 2017. We calculate an overall mass loss rate of <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">22</mn><mo>±</mo><mn mathvariant="normal">6</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="39pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="4b9e18a184893d4f6b000b93b280a068"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-35-2022-ie00001.svg" width="39pt" height="10pt" src="tc-16-35-2022-ie00001.png"/></svg:svg> Gt a −1 , corresponding to a sea level rise contribution of 0.06±0.02 mm a −1 . Compared to measurements prior to 2010, mass loss of glaciers on the Russian archipelagos has doubled in recent years. Article in Journal/Newspaper Arctic Climate change Franz Josef Land Novaya Zemlya Severnaya Zemlya The Cryosphere Directory of Open Access Journals: DOAJ Articles Arctic Franz Josef Land ENVELOPE(55.000,55.000,81.000,81.000) Severnaya Zemlya ENVELOPE(98.000,98.000,79.500,79.500) The Cryosphere 16 1 35 42
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
C. Sommer
T. Seehaus
A. Glazovsky
M. H. Braun
Brief communication: Increased glacier mass loss in the Russian High Arctic (2010–2017)
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description Glaciers in the Russian High Arctic have been subject to extensive atmospheric warming due to global climate change, yet their contribution to sea level rise has been relatively small over the past decades. Here we show surface elevation change measurements and geodetic mass balances of 93 % of all glacierized areas of Novaya Zemlya, Severnaya Zemlya, and Franz Josef Land using interferometric synthetic aperture radar measurements taken between 2010 and 2017. We calculate an overall mass loss rate of <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">22</mn><mo>±</mo><mn mathvariant="normal">6</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="39pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="4b9e18a184893d4f6b000b93b280a068"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-35-2022-ie00001.svg" width="39pt" height="10pt" src="tc-16-35-2022-ie00001.png"/></svg:svg> Gt a −1 , corresponding to a sea level rise contribution of 0.06±0.02 mm a −1 . Compared to measurements prior to 2010, mass loss of glaciers on the Russian archipelagos has doubled in recent years.
format Article in Journal/Newspaper
author C. Sommer
T. Seehaus
A. Glazovsky
M. H. Braun
author_facet C. Sommer
T. Seehaus
A. Glazovsky
M. H. Braun
author_sort C. Sommer
title Brief communication: Increased glacier mass loss in the Russian High Arctic (2010–2017)
title_short Brief communication: Increased glacier mass loss in the Russian High Arctic (2010–2017)
title_full Brief communication: Increased glacier mass loss in the Russian High Arctic (2010–2017)
title_fullStr Brief communication: Increased glacier mass loss in the Russian High Arctic (2010–2017)
title_full_unstemmed Brief communication: Increased glacier mass loss in the Russian High Arctic (2010–2017)
title_sort brief communication: increased glacier mass loss in the russian high arctic (2010–2017)
publisher Copernicus Publications
publishDate 2022
url https://doi.org/10.5194/tc-16-35-2022
https://doaj.org/article/5da1b74c26914c94aa11929261ae0dbe
long_lat ENVELOPE(55.000,55.000,81.000,81.000)
ENVELOPE(98.000,98.000,79.500,79.500)
geographic Arctic
Franz Josef Land
Severnaya Zemlya
geographic_facet Arctic
Franz Josef Land
Severnaya Zemlya
genre Arctic
Climate change
Franz Josef Land
Novaya Zemlya
Severnaya Zemlya
The Cryosphere
genre_facet Arctic
Climate change
Franz Josef Land
Novaya Zemlya
Severnaya Zemlya
The Cryosphere
op_source The Cryosphere, Vol 16, Pp 35-42 (2022)
op_relation https://tc.copernicus.org/articles/16/35/2022/tc-16-35-2022.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-16-35-2022
1994-0416
1994-0424
https://doaj.org/article/5da1b74c26914c94aa11929261ae0dbe
op_doi https://doi.org/10.5194/tc-16-35-2022
container_title The Cryosphere
container_volume 16
container_issue 1
container_start_page 35
op_container_end_page 42
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