Annual Glacier-Wide Mass Balance (2000–2016) of the Interior Tibetan Plateau Reconstructed from MODIS Albedo Products

Glaciers in the Tibetan Plateau (TP) play a crucial role in regulating agriculture irrigation, river discharge and the regional/global climate system. However, mass balance records of TP glaciers have remained scarce due to challenging mountainous terrain and harsh weather conditions, which limits o...

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Published in:Remote Sensing
Main Authors: Zhimin Zhang, Liming Jiang, Lin Liu, Yafei Sun, Hansheng Wang
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2018
Subjects:
Q
Online Access:https://doi.org/10.3390/rs10071031
https://doaj.org/article/61a4f03f3ade4cf2b1268deb709a2b58
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spelling ftdoajarticles:oai:doaj.org/article:61a4f03f3ade4cf2b1268deb709a2b58 2023-05-15T16:38:19+02:00 Annual Glacier-Wide Mass Balance (2000–2016) of the Interior Tibetan Plateau Reconstructed from MODIS Albedo Products Zhimin Zhang Liming Jiang Lin Liu Yafei Sun Hansheng Wang 2018-06-01T00:00:00Z https://doi.org/10.3390/rs10071031 https://doaj.org/article/61a4f03f3ade4cf2b1268deb709a2b58 EN eng MDPI AG http://www.mdpi.com/2072-4292/10/7/1031 https://doaj.org/toc/2072-4292 2072-4292 doi:10.3390/rs10071031 https://doaj.org/article/61a4f03f3ade4cf2b1268deb709a2b58 Remote Sensing, Vol 10, Iss 7, p 1031 (2018) glacier mass balance MODIS albedo Tibetan Plateau (TP) air temperature Science Q article 2018 ftdoajarticles https://doi.org/10.3390/rs10071031 2022-12-31T15:24:48Z Glaciers in the Tibetan Plateau (TP) play a crucial role in regulating agriculture irrigation, river discharge and the regional/global climate system. However, mass balance records of TP glaciers have remained scarce due to challenging mountainous terrain and harsh weather conditions, which limits our understanding of the influence of melting glaciers on local water resources and responses to climate change. Here, we present and assess an albedo-based method to derive annual mass balance for three glaciers in the interior TP from Moderate Resolution Imaging Spectroradiometer (MODIS) albedo data during 2000–2016. A strong linear correlation (R2 = 0.941, P < 0.001) is found between annual minimum-averaged glacier-wide albedo (AMGA) values and annual mass balance measurements on the Xiao Dongkemadi glacier. Furthermore, the 17-year-long annual mass balance series of the Xiao Dongkemadi glacier and the Geladandong mountain region glaciers, and the Purogangri ice cap are reconstructed for the first time, with a mass loss rate of 535 ± 63 mm w.e.a−1, 243 ± 66 mm w.e.a−1 and 113 ± 68 mm w.e.a−1, respectively. The results are verified by geodetic estimates, with relative error ranging from 4.55% to 11.80%, confirming that the albedo-based method can be used to estimate specific mass budgets for interior TP glaciers. A strong correlation between the mass balance series and air temperature infers that increasing summer air temperature may be one of main reasons for glacier shrinkage of the three studied glaciers. Article in Journal/Newspaper Ice cap Directory of Open Access Journals: DOAJ Articles Remote Sensing 10 7 1031
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic glacier mass balance
MODIS albedo
Tibetan Plateau (TP)
air temperature
Science
Q
spellingShingle glacier mass balance
MODIS albedo
Tibetan Plateau (TP)
air temperature
Science
Q
Zhimin Zhang
Liming Jiang
Lin Liu
Yafei Sun
Hansheng Wang
Annual Glacier-Wide Mass Balance (2000–2016) of the Interior Tibetan Plateau Reconstructed from MODIS Albedo Products
topic_facet glacier mass balance
MODIS albedo
Tibetan Plateau (TP)
air temperature
Science
Q
description Glaciers in the Tibetan Plateau (TP) play a crucial role in regulating agriculture irrigation, river discharge and the regional/global climate system. However, mass balance records of TP glaciers have remained scarce due to challenging mountainous terrain and harsh weather conditions, which limits our understanding of the influence of melting glaciers on local water resources and responses to climate change. Here, we present and assess an albedo-based method to derive annual mass balance for three glaciers in the interior TP from Moderate Resolution Imaging Spectroradiometer (MODIS) albedo data during 2000–2016. A strong linear correlation (R2 = 0.941, P < 0.001) is found between annual minimum-averaged glacier-wide albedo (AMGA) values and annual mass balance measurements on the Xiao Dongkemadi glacier. Furthermore, the 17-year-long annual mass balance series of the Xiao Dongkemadi glacier and the Geladandong mountain region glaciers, and the Purogangri ice cap are reconstructed for the first time, with a mass loss rate of 535 ± 63 mm w.e.a−1, 243 ± 66 mm w.e.a−1 and 113 ± 68 mm w.e.a−1, respectively. The results are verified by geodetic estimates, with relative error ranging from 4.55% to 11.80%, confirming that the albedo-based method can be used to estimate specific mass budgets for interior TP glaciers. A strong correlation between the mass balance series and air temperature infers that increasing summer air temperature may be one of main reasons for glacier shrinkage of the three studied glaciers.
format Article in Journal/Newspaper
author Zhimin Zhang
Liming Jiang
Lin Liu
Yafei Sun
Hansheng Wang
author_facet Zhimin Zhang
Liming Jiang
Lin Liu
Yafei Sun
Hansheng Wang
author_sort Zhimin Zhang
title Annual Glacier-Wide Mass Balance (2000–2016) of the Interior Tibetan Plateau Reconstructed from MODIS Albedo Products
title_short Annual Glacier-Wide Mass Balance (2000–2016) of the Interior Tibetan Plateau Reconstructed from MODIS Albedo Products
title_full Annual Glacier-Wide Mass Balance (2000–2016) of the Interior Tibetan Plateau Reconstructed from MODIS Albedo Products
title_fullStr Annual Glacier-Wide Mass Balance (2000–2016) of the Interior Tibetan Plateau Reconstructed from MODIS Albedo Products
title_full_unstemmed Annual Glacier-Wide Mass Balance (2000–2016) of the Interior Tibetan Plateau Reconstructed from MODIS Albedo Products
title_sort annual glacier-wide mass balance (2000–2016) of the interior tibetan plateau reconstructed from modis albedo products
publisher MDPI AG
publishDate 2018
url https://doi.org/10.3390/rs10071031
https://doaj.org/article/61a4f03f3ade4cf2b1268deb709a2b58
genre Ice cap
genre_facet Ice cap
op_source Remote Sensing, Vol 10, Iss 7, p 1031 (2018)
op_relation http://www.mdpi.com/2072-4292/10/7/1031
https://doaj.org/toc/2072-4292
2072-4292
doi:10.3390/rs10071031
https://doaj.org/article/61a4f03f3ade4cf2b1268deb709a2b58
op_doi https://doi.org/10.3390/rs10071031
container_title Remote Sensing
container_volume 10
container_issue 7
container_start_page 1031
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