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Analysis on the occurance regularity of high temperature disaster from June to September in recent 50a in Chongqing

机译:重庆近50A年6月至9月高温灾害发生规律性分析

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Taking the day numbers of daily average temperature ≥30°C and the day numbers of daily maximum temperature ≥35°C as the index of high temperature disaster, the occurrence regularity of high temperature disaster for June to September was analyzed from 1961 to 2010 in Chongqing. The results showed that there was a large inter-decadal variation in occurrence of high temperature disaster. The most severe year of high temperature disaster was the year of 2006, while the year of 1987 is the lightest one. The general trend was that it was the lowest one in the 1980s and gradually increased in the 1990s, and reached the highest value in the 2000s. The spatial distribution of the day numbers of daily average temperature ≥30°C was the same as that of the day numbers of daily maximum temperature ≥35°C. The highest values were distributed at the areas of Kaixian, Yunyang, Wushan in the Northeast part and Fengdu, Fuling in the middle part and Banan, Shapingba, Beibei in urban district and Qijiang in the southwest part. The lowest values were distributed at the areas of Xiushan, Youyang, Qianjiang in the southeast part and Chengkou, Fengjie in the northeast part and Dazu, Rongchang in the west part.
机译:以每日平均温度≥30°C的日子数量≥35°C作为高温灾害指数,从1961年至2010年分析了6月至9月的高温灾害的发生规律重庆。结果表明,高温灾害发生了大的间间变异。高温灾难最严重的一年是2006年,而1987年的年份是最轻的。一般趋势是,它是20世纪80年代最低的一个,并在20世纪90年代逐渐增加,并达到了2000年代的最高价值。每日平均温度≥30°C的白天数量的空间分布与日本最高温度≥35°C的日间数量相同。最高价值分布在东北部和冯德岛武山,涪陵中,涪陵,在西南部城区的中间部分和北城,北部,北宜。最低价值分布在秀山,酉阳,黔江在东南部和成都,奉杰,在东北部和大寨,荣昌在西部。

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