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Estimation of subpixel MODIS water temperature near coastlines using the SWTI algorithm

机译:使用SWTI算法估算海岸线附近的亚像素MODIS水温

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Satellite derived water surface temperature maps are widely used in many environmental studies and applications. The Moderate Resolution Imaging Spectroradiometer (MODIS) is among the widely used sensors in this field and sea surface temperature (SST) is one of the standard quantities derived fromMODIS imagery. However, MODIS SST maps have limited applications in near-shore and coastal environments due to inadequate spatial resolution of 1 km. This problem means that the MODIS pixels closer than 1 km from the shore aremixed pixels, i.e. they include by both water and land, and must be discarded from the SST map. In this work SWTI (Sharpening Water Thermal Imagery) methodswere applied toMODIS thermal imagery for the first time. The information required by SWTI regarding cover fractions and perpendicular vegetation index was obtained fromtheMODIS images in the Visible-Near Infrared bands at a spatial resolution of 250 m. In this way, the SST MODIS maps were extended to aminimumdistance of 250 mfrom the shore. The SWTI results were evaluated using as a reference the SST computed fromtwo ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) images acquired simultaneously to theMODIS images and covering the same areas. The applied validation methodology provides an evaluation of the deviations introduced by SWTI separated from the pre-existing differences between MODIS SST and ASTER SST upscaled to 250 m. For sea coast environments, SWTI was able to compute the SST of more than 80% of the pixels close to the shore at a spatial resolution of 250 m. This represents an increase of 67% compared to the number of pixels obtainable using a simple downscaling method based on polynomial interpolation; in areas with lagoons and estuaries the increases were +70% and +60% respectively. The ASTER SST comparison showed that the SST bias and the unsystematic deviation introduced by SWTI were Δ_S ≤ 0.45 K and σ(?_S) ≤ 0.88 K respectively, corresponding to a total deviation TD ≤ 0.97 K. SWTI is written in the IDL language and could be adapted for automatic application to MODIS images.
机译:卫星得出的水面温度图被广泛用于许多环境研究和应用中。中分辨率成像光谱仪(MODIS)是该领域中广泛使用的传感器之一,而海面温度(SST)是从MODIS图像得出的标准量之一。但是,由于1 km的空间分辨率不足,MODIS SST地图在近岸和沿海环境中的应用受到限制。这个问题意味着距离海岸不到1公里的MODIS像素是混合像素,即水和陆地都包含这些像素,必须将其从SST地图中丢弃。在这项工作中,SWTI(锐化水热成像)方法首次应用于MODIS热成像。 SWTI要求的有关覆盖率和垂直植被指数的信息是从可见光-近红外波段中的MODIS图像中以250 m的空间分辨率获得的。这样,SST MODIS地图被扩展到距海岸250 m的最小距离。 SWTI结果的评估以SST为参考,该SST是从同时获取到MODIS图像并覆盖相同区域的两个ASTER(先进星载热发射和反射辐射计)图像计算得到的。应用的验证方法可以评估SWTI引入的偏差,并将其与MODIS SST和ASTER SST之间的预先存在的差异(放大到250 m)分开。对于沿海环境,SWTI能够以250 m的空间分辨率计算靠近海岸的80%以上像素的SST。与使用基于多项式插值的简单降尺度方法可获得的像素数量相比,这意味着增加了67%;在有泻湖和河口的地区,增长率分别为+ 70%和+ 60%。 ASTER SST比较显示,SWTI引入的SST偏差和非系统偏差分别为Δ_S≤0.45 K和σ(?_ S)≤0.88 K,对应于总偏差TD≤0.97K。SWTI用IDL语言编写并可以适用于自动应用于MODIS图像。

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