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Climate change and sediment flux from the Roof of the World

机译:来自世界屋顶的气候变化和泥沙通量

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摘要

Potential rises in global temperature are likely to have major impacts on high altitude environments, including glacier recession and permafrost degradation. In turn, these could have far-reaching impacts on riverine sediment flux. Such impacts are emerging in the Himalayas and Tibet Plateau region, one of the world's largest and most environmentally-sensitive cold regions. Closer monitoring is urgently required to track changing trends of sediment load from the interactions of glacial recession treat, rainfall changes and human interventions, and to study the implications of such changes for the large Asian river systems of the region. Copyright (C) 2010 John Wiley & Sons, Ltd
机译:全球温度的潜在升高可能会对高海拔环境产生重大影响,包括冰川衰退和多年冻土退化。反过来,这些可能对河流沉积物通量产生深远的影响。在全球最大,对环境最敏感的寒冷地区之一的喜马拉雅山和西藏高原地区,这种影响正在显现。迫切需要进行更严密的监测,以追踪冰川消融,降雨变化和人为干预之间相互作用产生的泥沙负荷变化趋势,并研究这种变化对亚洲大型河流系统的影响。版权所有(C)2010 John Wiley&Sons,Ltd

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