Changing Climatic Conditions Affect Snow Cover in Annapurna Region of Nepal

Susmita Shrestha, D. Poudel, T. W. Duex, Rodney B. Yantis
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Abstract

Changing climatic conditions affecting the physical environment, hydrology, forest and wildlife, agriculture, and other sectors of the economy has become a major concern worldwide. The Annapurna Range in the Central Himalayas in Nepal is experiencing impacts of climate change on various fronts, including temperature increase and change in snow cover area (SCA). The objectives of this study were to assess spatio-temporal variation in temperature, precipitation, and SCA in the Annapurna massif and establish a relationship between these variables. This study analyzed the daily maximum and minimum temperature and precipitation records of six weather stations in the region, and performed a long-term analysis (1990–2020) of snow cover over Annapurna massif analysing Satellite images from the past three decades provided by satellite 5 through 8 of the Landsat program and Geographic Information System (GIS) technology. The SCA was determined through Landsat images using the Normalized Difference Snow Index (NDSI). Temperature analysis showed that the northeast (Chame) and northwest (Jomsom) parts of the massif were undergoing a consistent increase in average temperature at the rate of 0.07 and 0.03∘∘C per year, respectively. A north-south gradient was observed in total annual precipitation with total precipitation increasing in Ghandruk and Ranipauwa (Muktinath) at 50 mm and 4.8 mm per year, respectively, and decreasing in Manang Bhot at 4.7 mm per year. The precipitation events increased during spring in the west (Lete), northwest (Jomsom), and south (Ghandruk) of the massif, whereas it decreased in the north (Manang Bhot) and northeast (Chame) for all seasons. The SCA varied from 397 km22 to 1735 km22 with a significantly decreasing trend in December. There was a non-significant SCA increase during March, indicating that more snow coverage could appear in the spring in the future. These results could help local communities, government agencies, tourism industries, and other stakeholders develop resource management plans and climate change adaptation strategies.
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气候条件变化对尼泊尔安纳普尔纳地区积雪的影响
气候条件的变化影响着自然环境、水文、森林和野生动物、农业和其他经济部门,已成为全世界关注的一个主要问题。尼泊尔喜马拉雅山脉中部的安纳普尔纳山脉正经历气候变化的多方面影响,包括气温上升和积雪面积变化。本研究的目的是评估安纳普尔纳地块温度、降水和SCA的时空变化,并建立这些变量之间的关系。这项研究分析了该地区六个气象站的每日最高和最低温度和降水记录,并对安纳普尔纳地块的积雪进行了长期分析(1990-2020年),分析了陆地卫星计划的5号至8号卫星和地理信息系统技术提供的过去三十年的卫星图像。SCA是通过使用归一化差异雪指数(NDSI)的陆地卫星图像确定的。温度分析表明,该地块的东北部(Chame)和西北部(Jomsom)的平均温度分别以每年0.07和0.03摄氏度的速度持续上升。观察到年总降水量呈南北梯度,甘德鲁克和拉尼帕瓦(穆克蒂纳特)的总降水量分别以每年50毫米和4.8毫米的速度增加,马南布霍特的总降雨量以每年4.7毫米的速度减少。春季期间,该地块西部(莱特)、西北部(乔姆松)和南部(甘德鲁克)的降水事件增加,而北部(马南布霍特)和东北部(查梅)的降水量在所有季节都有所减少。SCA在397 km22至1735 km22之间变化,12月呈显著下降趋势。3月份SCA没有显著增加,这表明未来春季可能会出现更多的积雪。这些结果可以帮助当地社区、政府机构、旅游业和其他利益相关者制定资源管理计划和气候变化适应战略。
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来源期刊
Strategic Planning for Energy and the Environment
Strategic Planning for Energy and the Environment Environmental Science-Environmental Science (all)
CiteScore
1.50
自引率
0.00%
发文量
25
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