巴基斯坦主要气候带年和季节气候模式变化的时空评价

Haris Uddin Qureshi, Syed Muzzamil Hussain Shah, F. Teo
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摘要

气候变化对生态环境的广泛影响已成为当今人类面临的最大挑战之一。除时间尺度外,由于空间特征和纬度位置的不同,气候模式在空间尺度上也存在差异。这就需要调查不同地区不断变化的气候模式,以制定一项全面的气候变化适应和减缓战略。因此,本研究利用MK检验和Sen 's斜率估计方法,对1990-2022年巴基斯坦主要气候带的年和季节气候趋势进行了简要研究。研究结果表明,在研究期间,大喜马拉雅和亚山地地区的年平均气温上升约0.1 ~ 1.0°C,中部、南部和沿海地区的年平均气温上升约0.15 ~ 1.2°C,而西部高地地区的年平均气温下降趋势明显。从季节上看,春天是这个国家所有季节中最温暖的。夏季,大喜马拉雅和西部高地的气温呈下降趋势,而其他气候带的气温则有所上升。在冬季,大喜马拉雅地区和俾路支省北部的气温上升了约0.1至1.0摄氏度,沿海地区的气温上升了约0.1至0.2摄氏度。年降水量在大部分站点呈增加趋势,而夏季风在大喜马拉雅地区呈下降趋势,而其他区域呈明显的上升趋势,其中西部高地(100-300 mm)的增量最大,旁遮普中部和印度河下游平原的增量约为50-150 mm。对于冬季降水,大喜马拉雅地区呈现上升趋势(0.3-0.9 mm/年),而该国南部和沿海地区则呈现下降趋势。根据调查结果,确定了巴基斯坦的气候模式在空间尺度上有很大差异,因此有必要制定一项综合和有效的气候变化适应和减缓战略,以保护该国的自然资源。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spatio-temporal Assessment of Changing Annual and Seasonal Climate Patterns over the Major Climatic Zones of Pakistan
The extensive impacts of climate change on the ecology and the environment have made it one of the biggest challenges being faced by the humanity today. Apart from the temporal scale, the climate patterns also vary on the spatial scale due to the different spatial features and the latitudinal location. This necessitates investigating the changing climate patterns over the different locales to formulate a holistic climate change adaptation and mitigation strategy. Therefore, this study was conducted to briefly investigate the annual and seasonal climate trends over the major climatic zones of Pakistan during the period 1990-2022 using the MK test and Sen’s slope estimator method. The results obtained from the study showed an annual mean temperature rise of about 0.1 to 1.0 °C over the Greater Himalayas and sub-Montane region, and about 0.15 to 1.2 °C over the central, southern, and the coastal parts of the country, while a declining trend was found over the Western Highlands during the study period. Seasonally, the spring season was found to be the warmest among all seasons in the country. For the summer season, a declining trend was found over the Greater Himalayas and Western Highlands, while warming increased over the other climatic zones. For the winter season, the temperature rose by about 0.1 to 1.0 °C over the Greater Himalayas and northern Balochistan, and by about 0.1 to 0.2 °C over the coastal zones. For annual precipitation, an increasing trend was found over the majority of the selected stations, whereas for the summer monsoon, a declining trend was found over the Greater Himalayas, while the other zones witnessed a significant rising trend, with the highest increment noted over the Western Highlands (100-300 mm), and about 50-150 mm in central Punjab and the lower Indus plain. For winter precipitation, the Greater Himalayas observed an upward trend (0.3-0.9 mm/year), while the southern and coastal parts of the country witnessed a declining pattern. Based on the findings, it was established that the climate patterns have varied greatly on the spatial scale over Pakistan, which necessitates the formulation of an integrated and effective climate change adaptation and mitigation strategy for the conservation of natural resources in the country.
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