Comparison of recent rainfall trend in complex hilly terrain of sub-temperate region of Uttarakhand

Abstract

Agriculture in hill and mountain ecosystem is predominantly rainfed with common occurrence of moisture stress. Due to erratic rainfall and adverse topology in the Indian Himalaya Region (IHR), agricultural drought has become a prime concern. It is a natural disaster which evolves in time and their impacts generally last a long period of time. The present study attempts to characterize annual, seasonal and monthly temporal trend and rainfall pattern of 56 years long-term (1964-2019) and post-urbanization or recent (1980-2019) period using meteorological data of ICARVPKAS, Experimental Farm Hawalbagh, Almoraand Headquarter office, Almora observatory located in mid-Himalayan region of Uttarakhand state of India. Man-Kendall (α≤ 0.05; α≤ 0.10) test, Sen.’s slope and rainfall anomaly index (RAI) were employed for detecting trend, changes in magnitude of rainfall and identifying rainfall deficit year, respectively. The statistically significant (α≤ 0.05) decreasing trend was found during post-urbanization (1980-2019) with Sen.'s slope for pre-monsoon season (-2.38 mm/year) and annual rainfall (-7.26 mm/year) for Hawalbagh, while cold winter season shows statistically significant deceasing trend with Sen.'s slope (-2.00 mm/year) at Headquarter office, Almora. The decreasing trend in monsoon season (statistically significant at α≤ 0.10) was found during (1964-2019). However, both the station showed decreasing rainfall trend for pre-monsoon, post-monsoon, cold winter season and annual season. Results revealed that RAI analysis frequency of drought year was increasing in last 10 years.