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青藏高原东南部冰湖变化模式及其影响因素研究

Study of the patterns of variations in ice lakes and the factors influencing these changes on the southeastern Tibetan plateau.

作者信息

Mingwei Y U, Feng L I, Yonggang G U O, Libin S U, Deshun Q I N

机构信息

College of Water Conservancy and Civil Engineering, Tibet Agriculture and Animal Husbandry University, Nyingchi, 860000, China.

Research Center of Civil, Hydraulic and Power Engineering of Tibet, Nyingchi, 860000, China.

出版信息

Heliyon. 2024 Aug 15;10(16):e36406. doi: 10.1016/j.heliyon.2024.e36406. eCollection 2024 Aug 30.

Abstract

The ice lakes in the southeastern Qinghai-Tibet Plateau have exhibited a pronounced expansion against the backdrop of global warming, consequently amplifying the local risk of ice lake outburst disasters. However, surveys of ice lake changes in the entire region have consistently been incomplete due to the prevalent high cloud density. On the basis of Landsat remote sensing images and the Google Earth Engine (GEE) cloud computing platform, in this study, the full convolution segmentation algorithm is utilized to accurately and comprehensively map the regional distribution of ice lakes in southeastern Tibet at consistent time intervals in 1993, 2008, and 2023. Furthermore, the formation, distribution, and dynamic changes in these ice lakes are investigated. The numbers of ice lakes discovered in 1993, 2008, and 2023 were 2520, 3198, and 3877, respectively. These lakes covered areas of approximately 337.64 ± 36.86 km, 363.92 ± 40.90 km, and 395.74 ± 22.72 km, respectively. These ice lakes are located primarily between altitudes of 4442 m and 4909 m. The total area experienced an annual growth rate of approximately 0.57 % from 1993 to 2023. In the present study, the long-term variations in ice lakes in each district and county are examined. These findings indicate that between 1993 and 2023, the expansion of ice lakes was more pronounced in regions with a large number of marine glaciers. Notably, Basu County presented the highest annual growth rate of the ice lake population, at 6.23 %, followed by Bomi County, at 4.28 %, and finally, Zayul County, at 2.94 %. The accelerated shrinkage of marine glaciers induced by global warming is the primary driver behind the expansion of ice lakes. The results obtained from this research will enhance our overall understanding of the complex dynamics and mechanisms that govern the formation of ice lakes while also offering valuable perspectives on the potential risks linked to their expansion in this particular area.

摘要

在全球变暖的背景下,青藏高原东南部的冰湖呈现出显著扩张,从而加大了当地冰湖溃决灾害的风险。然而,由于该地区普遍云密度较高,对整个区域冰湖变化的调查一直不完整。基于Landsat遥感影像和谷歌地球引擎(GEE)云计算平台,本研究利用全卷积分割算法,在1993年、2008年和2023年的固定时间间隔内,准确、全面地绘制了西藏东南部冰湖的区域分布。此外,还对这些冰湖的形成、分布和动态变化进行了研究。1993年、2008年和2023年发现的冰湖数量分别为2520个、3198个和3877个。这些湖泊的面积分别约为337.64±36.86平方千米、363.92±40.90平方千米和395.74±22.72平方千米。这些冰湖主要位于海拔4442米至4909米之间。从1993年到2023年,总面积的年增长率约为0.57%。在本研究中,对各区县冰湖的长期变化进行了考察。这些发现表明,1993年至2023年期间,在大量海洋性冰川分布的地区,冰湖扩张更为明显。值得注意的是,八宿县冰湖数量的年增长率最高,为6.23%,其次是波密县,为4.28%,最后是察隅县,为2.94%。全球变暖导致海洋性冰川加速退缩是冰湖扩张的主要驱动因素。本研究结果将增进我们对冰湖形成复杂动态和机制的全面理解,同时也为该特定区域冰湖扩张相关潜在风险提供有价值的见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b8a2/11382195/c073cbfbd3e7/gr1.jpg

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