FY-3/VIRR卫星遥感数据反演省级区域蒸散量  

Modelling evapotranspiration in provincial regions based on FY-3/VIRR remote sensing data

作　　者：赵红[1] 赵玉金[1] 李峰[1] 张海波[1] 

机构地区：[1]山东省气候中心,济南250031

出　　处：《农业工程学报》2014年第13期111-118,F0004,共9页Transactions of the Chinese Society of Agricultural Engineering

基　　金：公益性行业(气象)科研专项(GYHY201306046);山东省气象局气象科学技术研究项目(2008sdqxz06;2010sdqxz04)资助

摘　　要：为了扩大气象卫星FY-3在科研、业务中的应用范围,将数据尽快用于遥感反演蒸散量业务工作中,根据FY-3/VIRR卫星通道特点,以山东为研究区域,基于地表能量平衡方程,结合地面气象要素,提出了利用FY-3卫星遥感数据进行区域蒸散反演的方法,建立了省级的区域逐日蒸散量估算系统。以2013年5月11日、8月20日、10月16日估算的日蒸散量为例,分析表明:基于FY-3/VIRR卫星反演的日蒸散量与利用Pen-man公式方法得到的数据对比,偏差分别为-0.19、-0.12和0.16 mm/d,相对偏差分别为10%、12%和11%;反演结果可准确揭示区域内不同地表覆盖类型的蒸散量的空间特点和差异性,结果较为合理;与同区域、同时段的EOS/MODIS蒸散产品进行对比分析表明:2种日蒸散产品的空间分布特征总体非常相似,相关系数在0.99以上,均方根差在0.36 mm以下,说明2种产品的一致性较好。利用中国新型自主研发的FY-3卫星资料估算蒸散量是可行的。In order to expand meteorological satellite FY-3 in scientific research, the application of remote sensing inversion of the data is needed for evapotranspiration studies. Based on FY-3/VIRR channel characteristics and use of Shandong as a case study area, we proposed to use FY-3 satellite remote sensing data for regional evapotranspiration inversion and to establish a provincial regional daily evapotranspiration estimation system based on the surface energy balance equation in combination with ground meteorological elements（ air temperature and wind speed）. To test our newly developed system for estimation of evapotranspiration, we used May 11, August 20, October 16, 2013 as our study dates. The results showed that evapotranspiration estimated from the inversion of the FY-3/VIRR data was respectively-0.19 mm/d,-0.12 mm/d, and 0.16 mm/d difference for the three tested dates as compared to the results obtained from the Penman equation. The relative deviation of the results between the two methods was 10%, 12% and 11% for the three tested dates, respectively. The tested results showed a better FY-3 data quality for the distribution patterns that reflected different types of surface evapotranspiration and features including the daily highest evapotranspiration in a variety of water surfaces. Followed by the types of water surface was the artificial influence of land uses such as arable land, urban, etc. The least affected by human activities for the evapotransiration was mainly natural vegetation and land cover types, such as woodlands, shrubs. The bare land had the lowest evapotranspiration inversion which accurately revealed the different land cover types in the area of evapotranspiration and the space characteristics and differences. Evapotranspiration spatial distribution of farmland has important implications for drought monitoring, irrigation, etc., It is necessary to conduct further analysis of cropland evaporation. Depending on grain yield, farmland can be divided into high, medium and low-yield fields. E

关 键 词：气象卫星 遥感 蒸散 FY-3 VIRR卫星 EOS MODIS 地表能量平衡 

分 类 号：S127[农业科学—农业基础科学]