Climate Change and Variability in the Northeastern Himalayan Region of India

Benjamin L Saitluanga, Gabriel Lalchhandama, P. Rinawma
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Abstract

Mountainous regions are considered highly vulnerable to the affects of climate change. The extent of change and variability of climatic parameters is still unexamined in many remote mountainous areas.  This paper aims in understanding the change in pattern of rainfall and temperature for a period of 30 years in Mizoram. The analysis of time series changing trend in climatic variables is carried out by using Coefficient of Variation (CV), Mann-Kendall (M-K) and Sen’s Slope estimator. The analysis reveals that high variation is observed for both the variables in all the decadal, three decadal and seasonal change. The CV analysis shows that the highest seasonal rainfall variation occurs during winter and the highest seasonal temperature variation occurs during spring. Mann-Kendall test shows a significant change in rainfall with November showing the highest negative trend of rainfall. The temperature trend analysis in the study also reveals drastic change of temperature. An understanding of climatic change, trend and variability helps in predicting for better natural resources from the susceptibility of climate change.
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印度喜马拉雅东北部地区的气候变化和变率
山区被认为极易受到气候变化的影响。在许多偏远山区,气候参数的变化程度和变率仍未得到检验。本文旨在了解30年来米佐拉姆邦降雨和温度模式的变化。利用变异系数(CV)、Mann-Kendall (M-K)和Sen 's Slope估计量对气候变量的时间序列变化趋势进行了分析。分析表明,在所有年代际、三年代际和季节变化中,两个变量都有较大的变化。CV分析表明,冬季降水量变化最大,春季气温变化最大。Mann-Kendall检验显示降雨量变化显著,其中11月降雨量呈最高负趋势。研究中的温度趋势分析也揭示了温度的剧烈变化。了解气候变化、趋势和变率有助于从气候变化的易感性中预测更好的自然资源。
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