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Mapping regional turbulent heat fluxes via variational assimilation of land surface temperature data from polar orbiting satellites

机译:通过来自极性轨道卫星的地表温度数据的变分同化来映射区域湍流热通量

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摘要

Estimation of turbulent heat fluxes by assimilating sequences of land surface temperature (LST) measurements into variational data assimilation (VDA) frameworks has been the subject of several studies. The VDA approaches estimate turbulent heat fluxes by minimizing the difference between LST observations and estimations from the heat diffusion equation. The VDA methods have been tested only with high temporal resolution LST observations (e.g., from geostationary satellites) when applied at regional scales. Geostationary satellites can capture the diurnal cycle of LST, but they have a relatively low spatial resolution and mainly focus on low latitudes. To overcome these shortcomings, this study assimilates high spatial resolution LST data from polar orbiting satellites (e.g., Moderate Resolution Imaging Spectroradiometer, MODIS) into the combined-source (CS) and dual-source (DS) VDA schemes. An expression is developed to obtain an a priori evaporative fraction (EF) estimate from leaf area index (LAI) or apparent thermal inertia (ATI). The a priori EF estimate is used as an initial guess in the VDA approach. The results indicate that the VDA method is able to find the optimal value of EF by assimilating the low-temporal resolution MODIS LST data. The predicted turbulent heat fluxes from VDA are compared with the measurements from the large-aperture scintillometer at three sites (Arou, Daman, and Sidaoqiao) in the Heihe River Basin (located in northwest China). The findings indicate that the CS and DS VDA models perform well in various hydrological and vegetative conditions. The three-site-average root mean square errors (RMSEs) of sensible and latent heat fluxes estimates from the CS scheme are 37.44 W m(-2) and 94.30 W m(-2), respectively. The DS model reduces the above mentioned RMSEs by 19.82% and 21.37%, respectively. Overall, the results show that using the a priori EF estimate from the proposed expression in the VDA approach eliminates the need for the high reso
机译:通过将陆地温度(LST)测量序列(LST)测量分化为变分数据同化(VDA)框架来估计湍流热通量已经是几项研究的主题。通过最小化来自热扩散方程的LST观察和估计之间的差异,VDA接近估计湍流热通量。当在区域尺度施用时,VDA方法仅在高时的时间分辨率LST观察(例如,来自地静止卫星)进行了测试。地静止卫星可以捕获LST的昼夜周期,但它们具有相对较低的空间分辨率,主要关注低纬度。为了克服这些缺点,本研究将来自极性轨道卫星(例如,适度分辨率成像分光镜,MODIS)的高空间分辨率LST数据吸收到组合源(CS)和双源(DS)VDA方案中。开发表达以获得来自叶面积指数(LAI)或表观热惯性(ATI)的优先蒸发级分(EF)估计。先验的EF估计用作VDA方法的初始猜测。结果表明,VDA方法能够通过同化低时间分辨率MODIS LST数据来找到E​​F的最佳值。将VDA的预测湍流热量与大孔径闪烁计的测量相比,在黑河流域(位于中国西北部)的三个地点(Arou,Daman和Sidaoqiao)中的大孔径闪烁计。结果表明,CS和DS VDA模型在各种水文和营养状况中表现出良好。来自CS方案的三点平均均方根误差(RMSE)与CS方案的估计分别为37.44WM(-2)和94.30Wm(-2)。 DS模型分别将上述RMS减少19.82%和21.37%。总体而言,结果表明,使用VDA方法中提出的表达式的先验EF估计消除了对高分辨率的需求

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  • 作者单位

    Beijing Normal Univ Sch Nat Resources Fac Geog Sci State Key Lab Earth Surface Processes &

    Resource 19 Xinjiekouwai St Beijing 100875 Peoples R China;

    Beijing Normal Univ Sch Nat Resources Fac Geog Sci State Key Lab Earth Surface Processes &

    Resource 19 Xinjiekouwai St Beijing 100875 Peoples R China;

    Univ Hawaii Manoa Dept Civil &

    Environm Engn Honolulu HI 96822 USA;

    Joint Ctr Satellite Data Assimilat College Pk MD USA;

    Beijing Normal Univ Sch Nat Resources Fac Geog Sci State Key Lab Earth Surface Processes &

    Resource 19 Xinjiekouwai St Beijing 100875 Peoples R China;

    Beijing Normal Univ Sch Nat Resources Fac Geog Sci State Key Lab Earth Surface Processes &

    Resource 19 Xinjiekouwai St Beijing 100875 Peoples R China;

    Univ Elect Sci &

    Technol China Sch Resources &

    Environm Ctr Informat Geosci Chengdu 611731 Sichuan Peoples R China;

    Chinese Acad Agr Sci Natl Hulunber Grassland Ecosyst Observat &

    Res St Inst Agr Resources &

    Reg Planning Beijing 100081 Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 环境监测;一般性问题;地球物理学;
  • 关键词

    Variational data assimilation; Land surface temperature; Sensible heat flux; Latent heat flux; MODIS;

    机译:变分数据同化;陆地温度;明智的热量通量;潜热通量;MODIS;

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