首页> 外文会议>Asian conference on remote sensing;ACRS 2007 >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:使用NOAA-AVHRR和LANDSAT-TM图像比较区域尺度的蒸散量:以也门共和国萨那盆地的干旱地区为例

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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:估算蒸散量(ET)对于理解并最终干预自然系统的水循环至关重要。 ET是在地方,区域和全球各级以及净初级生产力模型上影响气候变化的主要因素之一,但很难测量和预测。遥感不能直接测量蒸发蒸腾量(ET),但可以对蒸发分数(EF)进行合理的估算,蒸发率定义为蒸发量与可用能量之比。在这项研究中,结合了气象观测和遥感测量得出的光谱数据的表面能平衡方法被用于估算ET。修改后的(SEBAL)地面能量平衡算法已应用于N0AA-14卫星上的超高分辨率高分辨率辐射计(AVHRR)和Landsat专题测绘仪(TM)的数据,用于估算地表反照率,地表温度(T_0),归一化植被指数(NDVI),净辐射,土壤热通量和感热通量,以估算也门干旱和半干旱的也门萨那盆地的蒸散量和地表条件,于1998年6月1日。干旱地区,多山的地形,实际ET是根据卫星立交期间的现场数据计算得出的,并按像素逐像素积分24小时以进行每日ET分配,并将其与从AVHRR和TM数据获得的值进行比较。作为山区盆地,已尝试通过添加DEM信息来考虑地形影响以估算净辐射。结果,该盆地的每日ET图用于分析某些观测数据,例如辐射和地表温度,并与估计数据进行比较。结果表明,AVHRR具有一定的合理性。但是,由于TM的空间分辨率比AVHRR的空间分辨率好,因此TM数据可提供更好的结果。

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