Analysis of climate variables in the upper Amu Darya river basin in Tajikistan

A. Gulakhmadov
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Abstract

This article presents the results of the trend analysis of precipitation, maximum and minimum temperatures in the upstream of Amu Darya River Basin in Tajikistan. The result showed that in the south part of Tajikistan the trend of the summer and winter seasons indicate a positive and the temperature rises in summer and winter. In the north and central part of Tajikistan, there is also a positive trend in summer and winter with the exception of the Rasht and Murgab stations, where was recorded a decreasing trend in air temperature in summer. The eastern part of Tajikistan, where the high-altitude territory begins, the temperature trend shows that the summer period of the year becomes slightly cooler, and the winter period shows an increasing temperature trend, i.e. it is getting warmer. On the flat plain areas of Tajikistan, a relative increase in precipitation is observed, and the amount of precipitation in the high-mountain zone (eastern Pamir) decreases according to long-term data. This study shows pronounced climatic fluctuations in Tajikistan, changes in air temperature and precipitation conditions.
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塔吉克斯坦阿姆河上游流域气候变量分析
本文介绍了塔吉克斯坦阿姆河流域上游降水、最高和最低气温的趋势分析结果。结果表明:塔吉克斯坦南部夏冬季节变化趋势为正,夏季和冬季气温上升;在塔吉克斯坦北部和中部,除了Rasht和Murgab站外,夏季和冬季也有积极的趋势,那里的气温在夏季有下降的趋势。塔吉克斯坦东部是高海拔地区的起点,气温趋势表现为一年中夏季气温略有下降,冬季气温呈上升趋势,即变暖。塔吉克斯坦平原地区的降水相对增加,而高山带(帕米尔高原东部)的降水则减少。这项研究表明,塔吉克斯坦的气候波动明显,气温和降水条件也在变化。
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18
审稿时长
10 weeks
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