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Glacial mass balance changes in the Karakoram and Himalaya based on CMIP5 multi-model climate projections

机译:基于CMIP5多模式气候预测的喀喇昆仑山和喜马拉雅山冰川质量平衡变化

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摘要

The impact of future climate change on the glaciers in the Karakoram and Himalaya (KH) is investigated using CMIP5 multi-model temperature and precipitation projections, and a relationship between glacial accumulation-area ratio and mass balance developed for the region based on the last 30 to 40 years of observational data. We estimate that the current glacial mass balance (year 2000) for the entire KH region is -6.6 +/- 1 Gta(-1), which decreases about sixfold to -35 +/- 2 Gta(-1) by the 2080s under the high emission scenario of RCP8.5. However, under the low emission scenario of RCP2.6 the glacial mass loss only doubles to -12 +/- 2 Gta(-1) by the 2080s. We also find that 10.6 and 27 % of the glaciers could face 'eventual disappearance' by the end of the century under RCP2.6 and RCP8.5 respectively, underscoring the threat to water resources under high emission scenarios.
机译:使用CMIP5多模式温度和降水预测研究了未来气候变化对喀喇昆仑山和喜马拉雅山(KH)冰川的影响,并基于最近30年的发展,对该地区的冰川蓄积面积比与质量平衡之间的关系进行了研究。到40年的观测数据我们估计,整个KH地区的当前冰川质量平衡(2000年)为-6.6 +/- 1 Gta(-1),到2080年代下降到-35 +/- 2 Gta(-1)约六倍。 RCP8.5的高排放情景。但是,在RCP2.6的低排放情景下,到2080年代,冰川质量损失仅翻倍至-12 +/- 2 Gta(-1)。我们还发现,到本世纪末,在RCP2.6和RCP8.5下,分别有10.6%和27%的冰川可能面临“最终消失”,这突出说明了高排放情景下对水资源的威胁。

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