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Extensive and drastically different alpine lake changes on Asia's high plateaus during the past four decades

机译:在过去的四十年中,亚洲高原地区的高山湖泊发生了巨大变化

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摘要

Asia’s high plateaus are sensitive to climate change and have been experiencing rapid warming over the past few decades. We found 99 new lakes and extensive lake expansion on the Tibetan Plateau during the last four decades, 1970–2013, due to increased precipitation and cryospheric contributions to its water balance. This contrasts with disappearing lakes and drastic shrinkage of lake areas on the adjacent Mongolian Plateau: 208 lakes disappeared, and 75% of the remaining lakes have shrunk. We detected a statistically significant coincidental timing of lake area changes in both plateaus, associated with the climate regime shift that occurred during 1997/1998. This distinct change in 1997/1998 is thought to be driven by large-scale atmospheric circulation changes in response to climate warming. Our findings reveal that these two adjacent plateaus have been changing in opposite directions in response to climate change. These findings shed light on the complex role of the regional climate and water cycles and provide useful information for ecological and water resource planning in these fragile landscapes.
机译:亚洲的高原地区对气候变化非常敏感,并且在过去的几十年中一直在迅速升温。在1970-2013年的最后四个十年中,由于降水增加和冰冻圈对其水量平衡的贡献,我们在青藏高原发现了99个新的湖泊,并进行了广泛的湖泊扩张。与之形成鲜明对比的是,消失的湖泊和毗邻的蒙古高原的湖泊面积急剧萎缩:消失了208个湖泊,其余75​​%的湖泊都缩小了。我们检测到两个高原地区的湖面积变化具有统计意义的巧合时机,与1997/1998年期间发生的气候变化有关。据认为,1997/1998年的这一明显变化是由于气候变暖引起的大规模大气环流变化所致。我们的发现表明,响应气候变化,这两个相邻的高原一直朝着相反的方向变化。这些发现揭示了区域气候和水循环的复杂作用,并为这些脆弱景观中的生态和水资源规划提供了有用的信息。

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