喜马拉雅东部地区东拉通冰川气候参数降尺度及其评价

IF 0.7 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES Journal of Climate Change Pub Date : 2023-06-17 DOI:10.3233/jcc230010
Anubha Aggarwal, S. Anbukumar, A. Mandal
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引用次数: 0

摘要

本文利用喜马拉雅登山研究所(HMI)自动气象站(AWS)、Gangtok印度气象局(IMD)、Yuksum和era5再分析数据,利用月温度递减率和减均值的基本降尺度技术,构建了东拉通冰川的温度(T)序列。利用Gangtok IMD数据和缩小后的ERA5数据估算冰川降水(P)。采用局部比例因子法对P数据进行降尺度处理。利用卫星资料估算的0.180 km3(1962 - 2020)体积变化,构建了冰川的质量平衡(MB)序列。观测结果表明,冰川质量随T、气溶胶光学深度(AOD)(从1980年的0.1增加到2020年的0.2)和p的增加而减少,主要发生在气温较高的6 - 7 - 8月。这项研究非常重要,因为它使用了多个数据集以及从文献中提取的实地数据来研究气候对东拉通冰川的影响。在缺乏实地资料的情况下,本研究产生的数据可用于冰川的质量平衡预测。
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A Climate Change Study: Downscaling of Climatic Parameters and Their Assessment Over East Rathong Glacier of Eastern Himalayan Region
In this study monthly Temperature Lapse Rates and basic downscaling technique of subtracting means are used to construct temperature (T) series over East Rathong glacier by using multiple data sets from Automatic Weather Stations (AWS) at Himalayan Mountaineering Institute (HMI), Gangtok Indian Meteorological Department (IMD), Yuksum and ERA5reanalysis data. Precipitation (P) over glacier is estimated using Gangtok IMD data and downscaled ERA5 data. The P data is downscaled using local scaling factor method. Change in volume of 0.180 km3 (from 1962 to 2020) estimated using satellite data are used to construct Mass Balance (MB) series for the glacier. It is observed that the glacier is losing its mass with increasing T, Aerosol Optical Depth (AOD) (from 0.1 in 1980 to 0.2 in 2020), and increasing Pmainly during June-July-August months when temperatures are already high. This study is important as it used multiple data sets along with field data extracted from the literature to study climatic impacts on East Rathong glacier. Data generated from this study may be used in mass balance projection of the glaciers in the absence of field data.
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来源期刊
Journal of Climate Change
Journal of Climate Change METEOROLOGY & ATMOSPHERIC SCIENCES-
自引率
16.70%
发文量
18
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