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dc.contributor.authorBhattacharya, Atanu
dc.contributor.authorBolch, Tobias
dc.contributor.authorMukherjee, Kriti
dc.contributor.authorKing, Owen George Ahren
dc.contributor.authorKapitsa, Vassiliy
dc.contributor.authorNeckel, Niklas
dc.contributor.authorYao, Tandong
dc.identifier.citationBhattacharya , A , Bolch , T , Mukherjee , K , King , O G A , Kapitsa , V , Neckel , N & Yao , T 2021 , ' High Mountain Asian glacier response to climate revealed by multi-temporal satellite observations since the 1960s ' , Nature Communications , vol. 12 , 4133 .
dc.identifier.otherORCID: /0000-0002-8201-5059/work/96817669
dc.descriptionFunding: This study was supported by the Strategic Priority Research Program of Chinese Academy of Sciences (XDA20100300) and the Swiss National Science Foundation (200021E_177652/1). NN received funding from the European Union’s Horizon 2020 programme (No. 689443).en
dc.description.abstractKnowledge about the long-term response of High Mountain Asian glaciers to climatic variations is paramount because of their important role in sustaining Asian river flow. Here, a satellite-based time series of glacier mass balance for seven climatically different regions across High Mountain Asia since the 1960s shows that glacier mass loss rates have persistently increased at most sites. Regional glacier mass budgets ranged from −0.40 ± 0.07 m w.e.a−1 in Central and Northern Tien Shan to −0.06 ± 0.07 m w.e.a−1 in Eastern Pamir, with considerable temporal and spatial variability. Highest rates of mass loss occurred in Central Himalaya and Northern Tien Shan after 2015 and even in regions where glaciers were previously in balance with climate, such as Eastern Pamir, mass losses prevailed in recent years. An increase in summer temperature explains the long-term trend in mass loss and now appears to drive mass loss even in regions formerly sensitive to both temperature and precipitation.
dc.relation.ispartofNature Communicationsen
dc.subjectGE Environmental Sciencesen
dc.titleHigh Mountain Asian glacier response to climate revealed by multi-temporal satellite observations since the 1960sen
dc.typeJournal articleen
dc.contributor.institutionUniversity of St Andrews. Environmental Change Research Groupen
dc.contributor.institutionUniversity of St Andrews. Bell-Edwards Geographic Data Instituteen
dc.contributor.institutionUniversity of St Andrews. School of Geography & Sustainable Developmenten
dc.description.statusPeer revieweden

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