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Observational evidence of the cooling effect of agricultural irrigation in Jilin, China

机译:吉林省农业灌溉降温效果的观测证据

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China features the second largest irrigation area in the world. Several modeling studies on a global scale have shown the irrigation impact in China, but no direct observational evidence has been reported. In this paper, we evaluated the impact of irrigation on temperature in Jilin province, China, using meteorological and satellite observations. The results show that the temperature difference between highly and lightly irrigated sites is statistically significant and highly correlated to the effective irrigation area and crop sown area over the past 53 years. The magnitude of the difference in maximum air temperature was almost twice that of the difference in minimum air temperature. The linear regression coefficient of the time series difference in maximum air temperature was more than three times that of the minimum air temperature. Moreover, both meteorological and satellite observations show that the temperature difference is amplified during drier years. The difference in the magnitude of daytime land surface temperature (LST), between areas with irrigation percentages of more than 50 and less than 50, is as high as 2.7 K during the driest year. Overall, this study may provide evidence that an irrigation cooling effect exists in China.
机译:中国是世界第二大灌溉区。全球范围内的数项建模研究均显示了灌溉对中国的影响,但尚无直接观测证据的报道。在本文中,我们使用气象和卫星观测评估了吉林省灌溉对温度的影响。结果表明,过去53年中,高灌区和轻灌区之间的温差具有统计学意义,并且与有效灌溉面积和农作物播种面积高度相关。最高气温差的大小几乎是最低气温差的两倍。最高气温的时间序列差异的线性回归系数是最低气温的三倍以上。此外,气象和卫星观测都表明,在较干燥的年份中,温差会增大。在最干旱的年份,灌溉百分比大于50且小于50的区域之间的白天陆地表面温度(LST)的大小差异高达2.7K。总的来说,这项研究可以提供证据表明中国存在灌溉降温作用。

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