Glacier anomaly over the western Kunlun Mountains, Northwestern Tibetan Plateau, since the 1970s
Western Kunlun Mountain (WKM) glaciers show balanced or even slightly positive mass budgets in the early 21st century, and this is anomalous in a global context of glacier reduction. However, it is unknown whether the stability prevails at longer time scales because mass budgets have been unavailabl...
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Cambridge University Press
2018
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Online Access: | https://doi.org/10.1017/jog.2018.53 https://doaj.org/article/40b87f917ce94c73997e3eea49d793e4 |
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ftdoajarticles:oai:doaj.org/article:40b87f917ce94c73997e3eea49d793e4 2023-05-15T16:57:34+02:00 Glacier anomaly over the western Kunlun Mountains, Northwestern Tibetan Plateau, since the 1970s YETANG WANG SHUGUI HOU BAOJUAN HUAI WENLING AN HONGXI PANG YAPING LIU 2018-08-01T00:00:00Z https://doi.org/10.1017/jog.2018.53 https://doaj.org/article/40b87f917ce94c73997e3eea49d793e4 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143018000539/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2018.53 0022-1430 1727-5652 https://doaj.org/article/40b87f917ce94c73997e3eea49d793e4 Journal of Glaciology, Vol 64, Pp 624-636 (2018) glacier changes Tibetan plateau western Kunlun Mountains Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2018 ftdoajarticles https://doi.org/10.1017/jog.2018.53 2023-03-12T01:30:59Z Western Kunlun Mountain (WKM) glaciers show balanced or even slightly positive mass budgets in the early 21st century, and this is anomalous in a global context of glacier reduction. However, it is unknown whether the stability prevails at longer time scales because mass budgets have been unavailable before 2000. Here topographical maps, Shuttle Radar Topography Mission and Landsat data are used to examine the area and surface elevation changes of glaciers on the WKM since the 1970s. Heterogeneous glacier behaviors are observed not only in the changes of length and area, but also in the spatial distribution of surface elevation changes. However, on average, glacier area and elevation changes are not significant. Glaciers reduce in the area by 0.07 ± 0.1% a−1 from the 1970s to 2016. Averaged glacier mass loss is −0.06 ± 0.13 m w.e. a−1 from the 1970s to 1999. These findings show that the WKM glacier anomaly extends back at least to the 1970s. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 64 246 624 636 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
glacier changes Tibetan plateau western Kunlun Mountains Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
glacier changes Tibetan plateau western Kunlun Mountains Environmental sciences GE1-350 Meteorology. Climatology QC851-999 YETANG WANG SHUGUI HOU BAOJUAN HUAI WENLING AN HONGXI PANG YAPING LIU Glacier anomaly over the western Kunlun Mountains, Northwestern Tibetan Plateau, since the 1970s |
topic_facet |
glacier changes Tibetan plateau western Kunlun Mountains Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
Western Kunlun Mountain (WKM) glaciers show balanced or even slightly positive mass budgets in the early 21st century, and this is anomalous in a global context of glacier reduction. However, it is unknown whether the stability prevails at longer time scales because mass budgets have been unavailable before 2000. Here topographical maps, Shuttle Radar Topography Mission and Landsat data are used to examine the area and surface elevation changes of glaciers on the WKM since the 1970s. Heterogeneous glacier behaviors are observed not only in the changes of length and area, but also in the spatial distribution of surface elevation changes. However, on average, glacier area and elevation changes are not significant. Glaciers reduce in the area by 0.07 ± 0.1% a−1 from the 1970s to 2016. Averaged glacier mass loss is −0.06 ± 0.13 m w.e. a−1 from the 1970s to 1999. These findings show that the WKM glacier anomaly extends back at least to the 1970s. |
format |
Article in Journal/Newspaper |
author |
YETANG WANG SHUGUI HOU BAOJUAN HUAI WENLING AN HONGXI PANG YAPING LIU |
author_facet |
YETANG WANG SHUGUI HOU BAOJUAN HUAI WENLING AN HONGXI PANG YAPING LIU |
author_sort |
YETANG WANG |
title |
Glacier anomaly over the western Kunlun Mountains, Northwestern Tibetan Plateau, since the 1970s |
title_short |
Glacier anomaly over the western Kunlun Mountains, Northwestern Tibetan Plateau, since the 1970s |
title_full |
Glacier anomaly over the western Kunlun Mountains, Northwestern Tibetan Plateau, since the 1970s |
title_fullStr |
Glacier anomaly over the western Kunlun Mountains, Northwestern Tibetan Plateau, since the 1970s |
title_full_unstemmed |
Glacier anomaly over the western Kunlun Mountains, Northwestern Tibetan Plateau, since the 1970s |
title_sort |
glacier anomaly over the western kunlun mountains, northwestern tibetan plateau, since the 1970s |
publisher |
Cambridge University Press |
publishDate |
2018 |
url |
https://doi.org/10.1017/jog.2018.53 https://doaj.org/article/40b87f917ce94c73997e3eea49d793e4 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 64, Pp 624-636 (2018) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143018000539/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2018.53 0022-1430 1727-5652 https://doaj.org/article/40b87f917ce94c73997e3eea49d793e4 |
op_doi |
https://doi.org/10.1017/jog.2018.53 |
container_title |
Journal of Glaciology |
container_volume |
64 |
container_issue |
246 |
container_start_page |
624 |
op_container_end_page |
636 |
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1766049137120247808 |