首页> 外文会议>Asian conference on remote sensing >Comparison of Regional Scale Evapotranspiration using NOAA-AVHRR and LANDSAT- TM Images: A case study in an arid area in the Sana'a Basin, Republic of Yemen
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Comparison of Regional Scale Evapotranspiration using NOAA-AVHRR and LANDSAT- TM Images: A case study in an arid area in the Sana'a Basin, Republic of Yemen

机译:利用Noaa-AVHRR和Landsat-TM的区域规模蒸散的比较图像:也门Sana'a盆地干旱地区的案例研究

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Estimating evapotranspiration (ET) is of the highest importance for understanding and eventually intervening in the water cycle of natural systems. ET is one of the major factors influencing climate change, at local, regional and global levels, and net primary productivity models, but it is difficult to measure and predict. Remote sensing cannot provide a direct measurement of Evapotranspiration (ET), but it can provide a reasonably good estimate of the Evaporative Fraction (EF), defined as the ratio of ET and available energy. In this study, a surface energy balance method, which combines meteorological observations with spectral data derived from remote sensing measurements, was used to estimate the ET. The modified (SEBAL) Surface Energy Balance Algorithm for Land has been applied to data from the Advanced Very High Resolution Radiometer (AVHRR) onboard the N0AA-14 satellite and from the Landsat Thematic Mapper (TM) for the estimation of the surface albedo, surface temperature (T_0), normalized difference vegetation index (NDVI), net radiation, soil heat flux and sensible heat flux to estimate Evapotranspiration and surface conditions, on 1st June 1998 for the Sana'a Basin in Yemen, which is an arid and semi-arid region, with a mountainous terrain condition,. The actual ET was computed from field data during the satellite overpass and integrated for 24-h on a pixel-by-pixel basis for daily ET distribution and compared to the value obtained from the AVHRR and TM data. Being a mountainous basin, an attempt has been made to consider terrain effects in estimating net radiation by adding DEM information. As a result, a daily ET map over the Basin was used to analyze some observation data, such as radiation and surface temperature, and was compared with estimated data. The results showed that AVHRR gives some reasonable values; however, the TM data gives better results since the spatial resolution of TM is better than that of AVHRR.
机译:估算蒸散(ET)对于理解和最终干预自然系统的水循环是最重要的。 ET是影响气候变化的主要因素之一,在地方,区域和全球层面,净初级生产力模型,但难以衡量和预测。遥感不能提供蒸发(ET)的直接测量,但它可以提供与蒸发级分(EF)的合理估计,定义为ET和可用能量的比例。在该研究中,使用与遥感测量的光谱数据相结合的地表能量平衡方法,用于估计ET。用于土地的修改(Sebal)表面能量平衡算法已应用于来自高级高分辨率辐射计(AVHRR)的数据在N0AA-14卫星上,并从Landsat主题映射器(TM)估计表面Albedo,表面温度(t_0),归一化差异植被指数(NDVI),净辐射,土壤热量通量和明智的热量通量,以估算蒸发和表面条件,1998年6月1日在也门Sana'a盆地,这是一个干旱和半干旱地区,具有山地的地形条件。实际ET从卫星过桥期间的现场数据计算,并在每日ET分布的逐像素基础上集成24-H,并与从AVHRR和TM数据获得的值相比。作为一个山区盆地,通过添加DEM信息来考虑估算净辐射的地形效果。结果,盆地的每日ET映射用于分析一些观察数据,例如辐射和表面温度,并与估计数据进行比较。结果表明,AVHRR提供了一些合理的值;然而,由于TM的空间分辨率优于AVHRR的空间分辨率,TM数据提供了更好的结果。

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