蒙古阿尔泰山脉Tsambagarav山现代冰川动力学

Tuyagerel Davaagatan, A. Orkhonselenge
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引用次数: 0

摘要

本文研究了近40年来蒙古阿尔泰山脉Tsambagarav山的现代冰川动态。这是第一次对这一地块的冰川动力学进行回顾。利用归一化雪指数(归一化差雪指数)和归一化差主成分雪指数(归一化差主成分雪指数)估算了Tsambagarav山冰川面积的变化。利用Landsat多光谱扫描仪(MSS:分辨率为80 m)、Landsat专题成像仪(TM:分辨率为30 m)和Landsat业务陆地成像仪(OLI:分辨率为30 m)图像圈定的现代冰川的空间分布。结果表明,Tsambagarav山冰川面积从1977年的132.24 km2减少到2017年的63.92 km2,减少了51.7%。近40年来Tsambagarav山冰川面积的减少反映了现代冰川对气候变化的快速响应,即对太阳日照和/或当地和区域年平均气温的快速上升高度敏感。遥感数据和实地调查表明,现代冰川将在几十年内消失。该地块冰川的快速融化为蒙古西部的地表水资源提供了重要的资源。这项研究证明了在偏远地区进行空间分析对于了解现代冰川变化背景的重要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Modern glacier dynamics in Mt. Tsambagarav in the Mongolian Altai Mountain Range
This study presents the modern glacier dynamics in Mt. Tsambagarav in the Mongolian Altai Mountain Range over the last four decades. This is the first review of this type of glacier dynamics for this massif. Changes in glacier area in Mt. Tsambagarav are estimated using normalized indexes (Normalized Difference Snow Index and Normalized Difference Principal Component Snow Index). Spatial distribution of the modern glaciers delineated with Landsat Multispectral Scanner (MSS: resolution of 80 m), Landsat Thematic Mapper (TM: resolution of 30 m) and Landsat Operational Land Imager (OLI: resolution of 30 m) imageries. Result shows that Mt. Tsambagarav has lost 51.7% of the glacier area from 132.24 km2 in 1977 to 63.92 km2 in 2017. The loss in glacier area for Mt. Tsambagarav during the last 40 years reflect the rapid response of the modern glacier to climate change, i.e., it is highly sensitive to solar insolation and/or rapidly rising local and regional mean annual temperatures. The remote sensing data and field survey suggest that the modern glaciers would be disappeared on a scale of decades. Rapid melting of the glacier in this massif contributes to surface water resources in western Mongolia. This study demonstrates the importance of spatial analysis in the remote area for understanding the context of changes in the modern glaciers.
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来源期刊
CiteScore
0.70
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8 weeks
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