首页> 外文期刊>Agricultural and Forest Meteorology >Spatio-temporal variation of potential evapotranspiration and climatic drivers in the Jing-Jin-Ji region, North China
【24h】

Spatio-temporal variation of potential evapotranspiration and climatic drivers in the Jing-Jin-Ji region, North China

机译:华北京金吉地区潜在蒸发和气候司机的时空变化

获取原文
获取原文并翻译 | 示例
           

摘要

Potential evapotranspiration (ET0) is a key component of the water cycle and a main factor to water resources assessment. Analysis of variation inET0is significant in understanding the climate change and agricultural water management; It is affected by multiple climatic factors, including air temperature, relative humidity, wind speed, and sunshine duration. To understand the variations ofET0in the Jing-Jin-Ji region (Beijing Municipality, Tianjin Municipality, and Hebei Province), values ofET0and other climatic parameters at 22 national meteorological stations from 1961 to 2015 were analyzed. Cramer’s test showed a shift point in theET0data at approximately 1991. AnnualET0decreased from 1961 through 1991 at a rate of ?20.95?mm per decade, but annualET0increased at a rate of 7.40?mm per decade from 1992 to 2015. Partial correlation analysis and multiple linear regression methods were used to determine the dominant climatic driving factors forET0, and to reveal the causes of change inET0. From 1961 to 1991, the decrease of wind speed and sunshine duration offset the effect of increased air temperature, leading to reducedET0.However, from 1992 to 2015, average air temperature was the most dominant factor contributing to the increase inET0. Increased of air temperature and wind speed, and decreased relative humidity caused an increase inET0. This change inET0could impact hydrological cycle and agriculture irrigation management in the Jing-Jin-Ji region.
机译:潜在的蒸散(ETO)是水循环的关键组成部分和水资源评估的主要因素。在理解气候变化和农业水管理中的变异变异分析;它受到多气候因素的影响,包括空气温度,相对湿度,风速和阳光持续时间。要了解京锦吉地区(北京市,天津市,河北省),分析了1961年至2015年的22个国家气象站的ext0和其他气候参数的价值。 Cramer的考验在1991年,大约1991年到1991年的TheTeT0Data的转变点以1961年至1991年的每十年的速度为20.95毫秒,但从1992年到2015年的每十年率为7.40毫米的速度。部分相关性分析和多线性回归方法用于确定主要的气候驾驶因子5,并揭示变化的原因0。从1961年到1991年,风速和阳光持续时间的减少抵消了空气温度增加的效果,导致STAFTET0.从1992年到2015年,平均空气温度是导致INET增加最大的因素。增加空气温度和风速,并且相对湿度降低导致INET0增加。这种改变Inet0could在Jing-Jin-ji地区影响水文循环和农业灌溉管理。

著录项

  • 来源
    《Agricultural and Forest Meteorology》 |2018年第2018期|共9页
  • 作者单位

    State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin China Institute of Water Resources and Hydropower Research;

    State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin China Institute of Water Resources and Hydropower Research;

    State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin China Institute of Water Resources and Hydropower Research;

    State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin China Institute of Water Resources and Hydropower Research;

    Tianjin Key Laboratory of Water Resources and Environment Tianjin Normal University;

    State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin China Institute of Water Resources and Hydropower Research;

    State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin China Institute of Water Resources and Hydropower Research;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 other
  • 中图分类 农业基础科学;
  • 关键词

    Potential evapotranspiration; Climatic parameters; Shift point; Dominant factors; Jing-Jin-Ji region;

    机译:潜在的蒸散;气候参数;换档点;主导因素;景金吉地区;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号