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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Spatiotemporal patterns in the mean and extreme temperature indices of India, 1971-2005
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Spatiotemporal patterns in the mean and extreme temperature indices of India, 1971-2005

机译:1971-2005年印度平均温度和极端温度指数的时空分布

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This study provides the comprehensive analysis of changes in mean and extreme temperature indices of India to assist the climate change mitigation and adaptation strategies and to add information for the global comparisons, using a high-resolution daily gridded temperature data set (1? ×1?) during 1971-2005. In addition to the indices recommended by the World Meteorological Organization/CLIVAR Expert Team on Climate Change Detection and Indices, few more indices having social and agricultural implication are investigated at the seasonal and annual scales, utilizing widely adopted statistical methodologies in climate research. The results show, in general, a robust signal of warming, broadly consistent with what has been observed and predicted in other parts of the world in the context of global warming. The frequency and intensity of warm extremes, especially representing the daily minimum temperature, have increased with simultaneous decreases in cold extremes in large parts of the country, but the spatial distribution of the trend magnitude reflects the complex natural climatic settings of India and its possible interaction with the anthropogenic forcing. Seasonal analysis reveals a faster warming in day and night temperatures in winter affecting the major wheat crop. In summer, however, both human and ecosystems appear to be more vulnerable to the increasing tendency of the heatwave occurrences, particularly during night-time, since the 1990s. The relationship with the large-scale natural climatic modes indicates that the warming indices tend to increase in the year following the El Ni?o events as evident from the correlation with the NINO3.4 index, with a relatively higher association in the monsoon season. Moreover, the concurrent correspondence of the summer heatwaves with the north Indian Ocean sea surface temperature suggests a degree of predictability of the heat stress episode.
机译:本研究使用高分辨率的每日网格温度数据集(1?×1?1)来全面分析印度平均和极端温度指数的变化,以帮助缓解和适应气候变化的策略,并为全球比较添加信息。 )在1971-2005年期间。除了世界气象组织/ CLIVAR气候变化检测和指数专家组推荐的指数外,还利用气候研究中广泛采用的统计方法,在季节和年度尺度上对具有社会和农业影响的其他指数进行了调查。结果总体上显示出强烈的变暖信号,与全球变暖背景下世界其他地区已观察到并预测的信号大致相符。在该国大部分地区,极端天气的频率和强度(特别是代表每日最低气温的频率)和强度随着极端天气的同时下降而增加,但是趋势量的空间分布反映了印度复杂的自然气候环境及其可能的相互作用与人为强迫。季节性分析显示,冬季白天和晚上的气温升高较快,影响了主要小麦作物。但是,在夏季,自1990年代以来,尤其是在夜间,人类和生态系统似乎都更容易受到热浪发生的增加趋势的影响。与大规模自然气候模式的关系表明,在厄尔尼诺事件之后的一年中,变暖指数趋于增加,从与NINO3.4指数的相关性可以明显看出,季风季节的相关性相对较高。此外,夏季热浪与北印度洋海表温度的同时对应关系表明了热应力事件的可预测性。

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