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Projections of glacier change in the Altai Mountains under twenty-first century climate scenarios

机译:二十一世纪气候情景下的阿尔泰山冰川变化预测

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We project glacier surface mass balances of the Altai Mountains over the period 2006-2100 for the representative concentration pathway (RCP) 4.5 and RCP8.5 scenarios using daily near-surface air temperature and precipitation from 12 global climate models in combination with a surface mass balance model. The results indicate that the Altai glaciers will undergo sustained mass loss throughout the 21st for both RCPs and reveal the future fate of glaciers of different sizes. By 2100, glacier area in the region will shrink by 26 +/- A 10 % for RCP4.5, while it will shrink by 60 +/- A 15 % for RCP8.5. According to our simulations, most disappearing glaciers are located in the western part of the Altai Mountains. For RCP4.5, all glaciers disappearing in the twenty-first century have a present-day size smaller than 5.0 km(2), while for RCP8.5, an additional similar to 7 % of glaciers in the initial size class of 5.0-10.0 km(2) also vanish. We project different trends in the total meltwater discharge of the region for the two RCPs, which does not peak before 2100, with important consequences for regional water availability, particular for the semi-arid and arid regions. This further highlights the potential implications of change in the Altai glaciers on regional hydrology and environment.
机译:我们使用每日近地表气温和12种全球气候模型的降水量与地表质量相结合,对2006-2100年期间阿尔泰山脉的代表性地表径流(RCP)4.5和RCP8.5情景的冰川地表质量平衡进行了预测。平衡模型。结果表明,两个RCP的阿尔泰冰川将在21世纪持续遭受质量损失,并揭示出不同大小的冰川的未来命运。到2100年,RCP4.5的冰川面积将缩小26 +/- A 10%,而RCP8.5的冰川面积将缩小60 +/- A 15%。根据我们的模拟,大多数消失的冰川位于阿尔泰山脉的西部。对于RCP4.5,在二十一世纪消失的所有冰川的当前大小都小于5.0 km(2),而对于RCP8.5,在初始大小级别为5.0-2.5的冰川中,额外增加了约7%的冰川。 10.0 km(2)也消失了。我们预测了两个RCP区域的总融水排放量的不同趋势,该趋势在2100年之前没有达到峰值,这对区域的水资源供应(特别是半干旱和干旱地区)具有重要影响。这进一步凸显了阿尔泰冰川变化对区域水文学和环境的潜在影响。

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