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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Sub-pixel water temperature estimation from thermal-infrared imagery using vectorized lake features
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Sub-pixel water temperature estimation from thermal-infrared imagery using vectorized lake features

机译:使用矢量化湖特征从热红外图像估算亚像素水温

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摘要

Water skin temperature derived from thermal infrared satellite data are used in a wide variety of studies. Many of these studies would benefit from frequent, high spatial resolution (100 m pixels) thermal imagery but currently, at any given location, such data are only available every few weeks from spaceborne sensors such as ASTER. Lower spatial resolution (1 km pixels) thermal imagery is available multiple times per day at any given location, from several sensors such as MODIS on board both the AQUA and TERRA satellite platforms. In order to fully exploit lower spatial resolution imagery, a sub-pixel unmixing technique has been developed and tested at Quesnel Lake, British Columbia, Canada. This approach produces accurate, frequent high spatial resolution water skin temperature maps by exploiting a priori knowledge of water boundaries derived from vectorized water features. The pixel water-fraction maps are then input to a gradient descent algorithm to solve the mixed pixel ground leaving radiance equation for sub-pixel water temperature. Ground-leaving radiance is estimated from standard temperature and emissivity data products for pure pixels and a simple regression technique to estimate atmospheric effects. In this test case, MODIS 1 km thermal imagery was used along with 1:50,000 water features to create a high-resolution (100 m) water skin temperature map. This map is compared to a concurrent ASTER temperature image and found to be within 1 degrees C of the ASTER skin temperature 99% of the time. This is a considerable improvement over the 2.55 degrees C difference between the original MODIS product and ASTER image due to land temperature contamination. The algorithm is simple, effective, and unlocks a largely untapped resource for limnological and hydrological studies. (c) 2007 Elsevier Inc. All rights reserved.
机译:从热红外卫星数据得出的水皮肤温度被广泛用于各种研究中。这些研究中的许多研究将受益于频繁的,高空间分辨率(100 m像素)的热成像,但目前,在任何给定位置,此类数据仅每几周可从星载传感器(例如ASTER)获得。每天在任何给定位置均可通过多个传感器(例如AQUA和TERRA卫星平台上的MODIS)获得较低空间分辨率(1 km像素)的热图像。为了充分利用较低的空间分辨率图像,已经开发了亚像素分解技术,并在加拿大不列颠哥伦比亚省的奎斯内尔湖进行了测试。通过利用从矢量化水特征中得出的水边界的先验知识,该方法可以生成准确,频繁的高空间分辨率水皮肤温度图。然后将像素水分数图输入到梯度下降算法中,以求解混合像素地面,留下子像素水温的辐射方程。地面离地辐射率是根据纯像素的标准温度和发射率数据乘积以及一种简单的回归技术来估算大气影响来估算的。在此测试案例中,使用了MODIS 1 km热成像以及1:50,000的水特征来创建高分辨率(100 m)的水皮温度图。将该图与并发的ASTER温度图像进行比较,发现在99%的时间内,ASTER皮肤温度在1摄氏度以内。相对于原始MODIS产品和ASTER图像之间的2.55摄氏度的差异,这是一个很大的改进,这是由于地面温度受到污染所致。该算法简单,有效,并且可以释放大量尚未开发的资源用于水文和水文学研究。 (c)2007 Elsevier Inc.保留所有权利。

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