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Trend Analysis of Temperature Data for the Narayani River Basin, Nepal

Graduate School of Environmental Science, Hokkaido University, Hokkaido 060-0810, Japan
Department of Geosciences, University of Oslo, Blindern, 0316 Oslo, Norway
Department of Hydrology and Meteorology, Government of Nepal, Kathmandu 44600, Nepal
Geographic Information Systems (GIS) Area, NIIT University, Rajasthan 301705, India
Author to whom correspondence should be addressed.
Received: 21 February 2019 / Revised: 4 December 2020 / Accepted: 15 December 2020 / Published: 22 December 2020
The study of spatiotemporal variation in temperature is vital to assess changes in climate, especially in the Himalayan region, where the livelihoods of billions of people living downstream depends on water coming from the melting of snow and glacier ice. To this end, temperature trend analysis is carried out in the Narayani River basin, a major river basin of Nepal, characterized by three climatic regions: tropical, subtropical and alpine. Temperature data from six stations located within the basin were analyzed. The elevation of these stations ranges from 460 to 3800 m a.s.l. and the time period of available temperature data ranges from 1960–2015. Multiple regression and empirical mode decomposition (EMD) methods were applied to fill in missing data and to detect trends. Annual as well as seasonal trends were analyzed and a Mann–Kendall test was employed to test the statistical significance of detected trends. The results indicate significant cooling trends before 1970s, and warming trends after 1970s in the majority of the stations. The warming trends range from 0.028 to 0.035 °C year1 with a mean increasing trend of 0.03 °C year1 after 1971. Seasonal trends show the highest warming trends in the monsoon season, followed by winter and the premonsoon and postmonsoon season. However, the difference in warming rates between different seasons was not significant. An average temperature lapse rate of −0.006 °C m1 with the steepest value (−0.0064 °C m1) in the premonsoon season and the least negative (−0.0052 °C m1) in the winter season was observed for this basin. A comparative analysis of the gap-filled data with freely available global climate dataset show reasonable correlation, thus confirming the suitability of the gap filling methods. View Full-Text
Keywords: climate change; temperature trend; Himalaya; river basin; Nepal climate change; temperature trend; Himalaya; river basin; Nepal
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MDPI and ACS Style

Chand, M.B.; Bhattarai, B.C.; Pradhananga, N.S.; Baral, P. Trend Analysis of Temperature Data for the Narayani River Basin, Nepal. Sci 2021, 3, 1.

AMA Style

Chand MB, Bhattarai BC, Pradhananga NS, Baral P. Trend Analysis of Temperature Data for the Narayani River Basin, Nepal. Sci. 2021; 3(1):1.

Chicago/Turabian Style

Chand, Mohan B., Bikas C. Bhattarai, Niraj S. Pradhananga, and Prashant Baral. 2021. "Trend Analysis of Temperature Data for the Narayani River Basin, Nepal" Sci 3, no. 1: 1.

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