The Tibetan Plateau (TP) has warmed at a rate twice the global average and presents unique warming patterns in surface temperature changes. However, key characteristics of glacier surface heatwave duration and intensity over the TP during the present extreme warming period are still unknown. In this study, we show that surface temperatures in glacial regions of the TP (0.37 ± 0.10°C per decade) have increased faster than those in non‐glacial areas (0.29 ± 0.05°C per decade) between 2001 and 2020. Moreover, the duration (5.3 ± 3.2 days per decade) and cumulative intensity (24.9 ± 16.3 days °C per decade) of glacier surface heatwaves have increased significantly during autumn. Our results demonstrate an elevation dependence to these key warming characteristics, which we also suggest are associated with extreme glacier mass loss. Here, we highlight potential threats to the sustainability of glacier water resources and increasing risk of glacier related hazards at the “roof of the world.”
Glacier Surface Heatwaves Over the Tibetan Plateau
Wenfeng Chen,T. Yao,Guoqing Zhang,R. Woolway,Wei Yang,Fenglin Xu,Tao Zhou
Published 2023 in Geophysical Research Letters
ABSTRACT
PUBLICATION RECORD
- Publication year
2023
- Venue
Geophysical Research Letters
- Publication date
2023-03-15
- Fields of study
Not labeled
- Identifiers
- External record
- Source metadata
Semantic Scholar
CITATION MAP
EXTRACTION MAP
CLAIMS
- No claims are published for this paper.
CONCEPTS
- No concepts are published for this paper.
REFERENCES
Showing 1-83 of 83 references · Page 1 of 1
CITED BY
Showing 1-27 of 27 citing papers · Page 1 of 1