尼泊尔拉拉湖和贝格纳斯湖的湖泊流域动态和水深模拟

Eearth Pub Date : 2021-06-05 DOI:10.3390/EARTH2020016
S. Thakuri, Furbe Lama, R. Malla, Nitesh Khadka, N. Ghimire, F. Salerno
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引用次数: 1

摘要

湖泊演变及其随时间的变化是山区人类活动和气候变化影响的一个明显且易于测量的信号。本研究介绍了位于尼泊尔两个不同地理环境的永久性湖泊(贝格纳斯湖和拉拉湖)的水深模型。此外,还评估了湖泊流域土地覆盖和土壤侵蚀的时间变化,以及这些湖泊周围的气候趋势。本研究支持建立参考点,以探索人为和气候变化对湖泊水文系统影响的科学证据。二阶多项式模型最能反映湖泊深度与体积之间的关系。2019年,拉拉湖最大深度为169米,面积为10.52平方公里,水量为1013305万立方米(Mm3),而贝格纳斯湖最大深度为12.5米,面积为2.98±0.10平方公里,水量为13.539 Mm3。这两个湖区正在经历温度和降雨的变化。近几十年来,即使土地覆盖变化很小,拉拉湖及其流域的面积和体积也相对稳定。在过去的几十年里,贝格纳斯湖及其流域经历了重大变化。本研究认为,人类活动是贝格纳斯湖流域湖泊面积变化的主要原因,而不是气候变化。
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Lake Watershed Dynamics and Bathymetry Modeling of Rara and Begnas Lakes in Nepal
Lake evolution and its changes over time are an evident and easily measurable signal of human activities and climate change impacts in mountain regions. This study presents bathymetric modeling of permanent lakes (Begnas and Rara Lakes) located in two different geographic settings of Nepal. Moreover, temporal changes in land cover and soil erosion of the lake watersheds, as well as climatic trends around these lakes, are assessed. This study supports establishing reference sites for exploring scientific evidence on the impacts of anthropogenic and climate change on lake hydrological systems. Second-order polynomial models best represent the relationship between lake depth and volume. Rara Lake had a maximum depth of 169 m with an area of 10.52 km2 and a volume of 1013.305 million cubic meters (Mm3), whereas Begnas Lake had a maximum depth of 12.5 m with an area of 2.98 ± 0.10 km2 and a water volume of 13.539 Mm3 in the year 2019. Both lake regions are experiencing changes in temperature and rainfall. The area and volume of Rara Lake and its watershed have been relatively stable even with minimal land-cover change during the recent decades. Begnas Lake and its watershed have experienced significant changes in the last few decades. This study concludes that human activities in the Begnas Lake watersheds are the primary source of lake area variation rather than climate change.
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