首页> 外文会议>IEEE International Geoscience and Remote Sensing Symposium >Mapping land surface fluxes using microwave and optical remote sensing data under high vegetation cover conditions during SMEX02/SMACEX
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Mapping land surface fluxes using microwave and optical remote sensing data under high vegetation cover conditions during SMEX02/SMACEX

机译:使用微波和光学遥感数据在SMEx02 / SMACEx期间使用微波和光学遥感数据进行映射陆地表面通量

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A two-source (soil + vegetation) energy balance model using microwave-derived near-surface soil moisture has been successfully applied in areas of relatively low vegetation cover. The utility of this approach in areas with high vegetation cover is explored and compared with a two-source scheme using thermal infrared data. The investigation used data collected over areas of high corn and soybean cover in central Iowa during the Soil Moisture Experiment in 2002 (SMEX02) and the Soil Moisture Atmosphere Coupling Experiment (SMACEX). Maps of near-surface soil moisture data were obtained from the Polarimetric Scanning Radiometer (PSR) observations, which provided 800 m resolution for the regional area. Fractional vegetation cover and leaf area index were estimated from the Landsat data, which also provided surface temperature. These data, along with local meteorological data, provided inputs for a two-source model. The model output using microwave data were compared with tower-based flux measurements in the watershed area. The model computed reliable estimates of net radiation and soil heat flux, yielding a root-mean-square-difference (RMSD) of around 20 Wm/sup -2/. However, the model generally underestimated latent heat flux, LE, and overestimated sensible heat flux, H resulting in RMSD values of /spl sim/70 Wm/sup -2/ for LE and 45 Wm/sup -2/ for H respectively. The larger discrepancies in heat fluxes are due in part to the mismatch in model output resolution (800 m) versus source area contributing to the tower fluxes (/spl sim/100m). The comparison between the model output of surface temperature and Landsat indicates that the temperature estimation is reasonable agreement with a RMSD 1.4/spl deg/C. A comparison of fluxes mapped over the regional area using the microwave-based and thermal-infrared based model is made and factors contributing to the differences between model outputs are discussed.
机译:使用微波衍生的近表面土壤水分的双源(土壤+植被)能量平衡模型已成功应用于相对较低的植被覆盖区域。探索了这种方法在具有高植被覆盖的区域的效用,并与使用热红外数据的双源方案进行比较。 2002年土壤水分实验期间(SMEx02)和土壤水分气氛耦合实验(SMACEx),在伊瓦河中部伊瓦河中央和大豆覆盖区域采集了对高玉米和大豆覆盖的数据。从偏振扫描辐射计(PSR)观察中获得近表面土壤水分数据的地图,为区域区域提供800米的分辨率。估计分数植被覆盖和叶面积指数来自Landsat数据,也提供了表面温度。这些数据以及局部气象数据,为双源模型提供了输入。将使用微波数据的模型输出与流域区域的基于塔的磁通测量进行了比较。该模型计算了净辐射和土壤热通量的可靠估计,产生了大约20Wm / sup-2 /的根平均差(RMSD)。然而,模型通常低估了潜热通量,LE和高次曝光的显热通量,H分别导致/ SPL SIM / 70Wm / sup -2 / for 45 wm / sup -2 / for h的RMSD值。热量通量的较大差异部分是由于模型输出分辨率(800米)与塔磁通(/ SPL SIM / 100m)有贡献的源区的错配。表面温度和LANDSAT的模型输出之间的比较表明温度估计与RMSD 1.4 / SPL DEG / C具有合理的一致性。使用基于微波和热红外模型在区域区域上映射的助焊剂的比较,并讨论了对模型输出之间的差异的因素。

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