Arid
稻田逐时蒸散量的测定及其模拟方法的比较
其他题名Measurement Simulation of Hourly Evapotranspiration in Paddy Field with Different Methods
刘斌1; 胡继超1; 张雪松2; 张富存2
来源期刊灌溉排水学报
ISSN1672-3317
出版年2014
卷号33页码:369-373
中文摘要水稻生长季内,采用蒸渗计、涡度相关仪(EC)测定稻田逐时蒸散量,应用Penman-Monteith模型(PM模型)、Shuttleworth- Wallace双源模型(SW模型)进行模拟,并对比模拟值与观测值,验证了蒸散模型可靠性。结果表明:①涡度相关仪测定的稻田蒸散显著低于蒸渗计,蒸渗计测定的稻田蒸散较涡度相关法更为可靠。②SW模型模拟效果优于PM模型,模拟值与蒸渗计实测值更加接近,尤其在生育前期和后期水稻冠层稀疏时段。③稻田土壤蒸发占总蒸散比例较小且水层作用使阻力基数值降低,土壤阻力敏感性较旱地低。
英文摘要Hourly evapotranspiration in paddy field was observed directly by lysimeter and eddy covariance method (EC),and was simulated with using Penman-Monteith(PM) equation and Shuttleworth-Wallace (SW) model,respectively. The reliabilities of the two models were verified through comparing the observed and simulated evapotranspiration. The results showed that ① the measured evapotranspiration by EC were obvious lower compared with the lysimeter in each rice growth stage, and the reliability of measured evapotranspiration by lysimerter was higher.② The simulated effect of Shuttleworth-Wallace model was better than Penman-Monteith equation, and the simulated evapotranspiration was closer to the measured evapotranspiration by lysimeter, especially during the periods with sparse canopy.③Soil evaporation had a lower proportion in total evapotranspiration as well as a smaller resistance because of the water in the paddy,and the sensitivity of soil resistance was smaller than that in arid regions.
中文关键词逐时蒸散 ; 蒸渗计 ; Shuttleworth-Wallace双源模型 ; 稻田
英文关键词hourly evapotranspiration lysimeter shuttleworth-wallace model paddy field
语种中文
国家中国
收录类别CSCD
WOS类目METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向Meteorology & Atmospheric Sciences
CSCD记录号CSCD:5219016
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/231291
作者单位1.南京信息工程大学生态气象环境研究中心, 江苏省农业气象重点实验室, 南京, 江苏 210044, 中国;
2.江苏省农业气象重点实验室, 江苏省农业气象重点实验室, 南京, 江苏 210044, 中国
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GB/T 7714
刘斌,胡继超,张雪松,等. 稻田逐时蒸散量的测定及其模拟方法的比较[J],2014,33:369-373.
APA 刘斌,胡继超,张雪松,&张富存.(2014).稻田逐时蒸散量的测定及其模拟方法的比较.灌溉排水学报,33,369-373.
MLA 刘斌,et al."稻田逐时蒸散量的测定及其模拟方法的比较".灌溉排水学报 33(2014):369-373.
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