Characterizing the Climate of Tarai Region of Uttarakhand Based On Water Balance Studies

Shubhika Goel, Jaya Dhami, R K Singh
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Abstract

This research had been conducted for calculation of water balance components by Thornthwaite Mather method and simulation model WATBAL model had been used to calculate different water balance components like soil moisture, actual evapotranspiration, surplus, deficit, moisture adequacy index and soil moisture index by using average weekly precipitation and potential evapotranspiration from 1981-2020 for Tarai region of Uttarakhand. In this study, different weather-based indices like, Humidity Index, Aridity Index and Moisture Index also been calculated on the seasonal and annual basis. Based on which climatic classification had been done for Tarai region of Uttarakhand as well as it is of International significance as based on this study water stress condition for the crops and advisories could be done to the farmers for the Tarai region of the world. From, this study it has been concluded that humid climate exists in this region. The results also revealed that there is an increase in the water surplus during 1981-2020 when compared with IMD data for Pantnagar during 1971-2005. Water Surplus was found to be 670.0 mm and water deficit was found to be 440.2 mm. Total potential evapotranspiration was found to be 1339.4 mm, which was calculated by Penman Monteith’s equation during 1981-2020 and was found to be decreased when compared with the PET calculated by IMD for the year 1971-2005 of about 1463.9 mm. When compared with the IMD data over the periods from 1971-2005 with current data from 1981-2020 for Pantnagar region then humidity index had been decreased from 149.0% to 144.7% respectively. Aridity index had been decreased from 73.0% to 50.2%, as water deficit had been decreased from 566.7 mm to 440.2 mm. Moisture index had been increased from 76% to 94.5% as water surplus was increased from 447.7 mm to 670.0 mm respectively on annual basis.
基于水平衡研究的北阿坎德邦塔莱地区气候特征
本研究采用Thornthwaite Mather方法计算水分平衡分量,利用模拟模型WATBAL模型,利用1981-2020年平均周降水量和潜在蒸散量,计算了北阿克德邦塔拉伊地区土壤水分、实际蒸散量、富余、亏缺、水分充足指数和土壤水分指数等水分平衡分量。在本研究中,湿度指数、干燥指数和湿度指数等不同的基于天气的指数也按季节和年计算。在此基础上,对北阿坎德邦的塔莱地区进行了气候分类,并且具有国际意义,因为基于这项研究,作物的水分胁迫条件和可以向世界塔莱地区的农民提供建议。研究结果表明,该地区存在湿润气候。结果还表明,与1971-2005年的IMD数据相比,1981-2020年Pantnagar的水分盈余有所增加。水分过剩为670.0 mm,水分亏缺为440.2 mm。总潜在蒸散量为1339.4 mm(按Penman Monteith公式计算1981—2020年),与1971—2005年IMD计算的PET相比减少了1463.9 mm。与1971-2005年的IMD资料和1981-2020年的现期资料比较,Pantnagar地区的湿度指数分别从149.0%下降到144.7%。干旱指数由73.0%降至50.2%,水分亏缺由566.7 mm降至440.2 mm。水分指数从76%增加到94.5%,水分盈余从447.7 mm增加到670.0 mm。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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