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SPARC: New Cloud, Snow, and Cloud Shadow Detection Scheme for Historical 1-km AVHHR Data over Canada

机译:SPARC:针对加拿大1公里历史AVHHR数据的新云,雪和云阴影检测方案

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The identification of clear-sky and cloudy pixels is a key step in the processing of satellite observations. This is equally important for surface and cloud-atmosphere applications. In this paper, the Separation of Pixels Using Aggregated Rating over Canada (SPARC) algorithm is presented, a new method of pixel identification for image data from the Advanced Very High Resolution Radiometer (AVHRR) on board the NOAA satellites. The SPARC algorithm separates image pixels into clear-sky and cloudy categories based on a specially designed rating scheme. A mask depicting snow/ice and cloud shadows is also generated. The SPARC algorithm has been designed to work year-round (day and night) over the temperate and polar regions of North America, for current and historical AVHRR/NOAA High-Resolution Picture Transmission (HRPT) and Local Area Coverage (LAC) data with original 1-km spatial resolution. The algorithm was tested and applied to data from the AVHRR sensors flown on board NOAA-6 to NOAA-18. The method was employed in generating historical clear-sky composites for the 1982-2005 period at daily, 10-day, and monthly time scales at 1-km resolution for an area of 5700 km × 4800 km centered over Canada. This region also covers the northern part of the United States, including Alaska, as well as Greenland and the surrounding oceans. The SPARC algorithm is designed to produce an aggregated rating that accumulates the results of several tests. The magnitude of the rating serves as an indicator of the probability for a pixel to belong to the clear-sky, partly cloudy, or overcast categories. The individual tests employ the spectral properties of five AVHRR channels, as well as surface skin temperature maps from the North American Regional Reanalysis (NARR) dataset. These temperature fields are available at 32 km × 32 km spatial resolution and at 3-h time intervals. Combining all test results into one final rating for each pixel is beneficial for the generation of multiscene clear-sky composites. The selection of the best pixel to be used in the final clear-sky product is based on the magnitude of the rating. This provides much-improved results relative to other approaches or "yeso" decision methods. The SPARC method has been compared to the results of supervised classification for a number of AVHRR scenes representing various seasons (snow-free summer, winter with snow/ice coverage, and transition seasons). The results show an overall agreement between the automated (SPARC) and the supervised classification at the level of 80% to 91%.
机译:晴空像素的识别是卫星观测处理中的关键步骤。这对于地表和云大气应用同样重要。在本文中,提出了使用加拿大总体评级的像素分离(SPARC)算法,该算法是NOAA卫星上的超高分辨率高分辨率辐射计(AVHRR)图像数据的像素识别新方法。 SPARC算法根据特殊设计的分级方案将图像像素分为晴空和多云类别。还会生成描绘雪/冰和云阴影的蒙版。 SPARC算法旨在在北美温带和极地地区全年(白天和黑夜)工作,以获取当前和历史的AVHRR / NOAA高分辨率图片传输(HRPT)和局部区域覆盖(LAC)数据,以及原始的1公里空间分辨率。测试了该算法,并将其应用于从NOAA-6板载到NOAA-18上的AVHRR传感器的数据。该方法用于以加拿大全国为中心的5700 km×4800 km区域,以1 km的分辨率在1982、2005年期间以每天,10天和每月的时间尺度生成历史晴空合成图像。该地区还覆盖了美国北部,包括阿拉斯加,格陵兰和周围的海洋。 SPARC算法旨在产生汇总等级,该等级汇总了几次测试的结果。等级的大小用作像素属于晴空,部分多云或阴天类别的概率的指标。各个测试使用了五个AVHRR通道的光谱特性,以及来自北美区域再分析(NARR)数据集的表面皮肤温度图。这些温度场的空间分辨率为32 km×32 km,间隔时间为3小时。将所有测试结果合并为每个像素的最终评级,对于生成多场景晴空复合材料很有帮助。在最终晴空产品中使用的最佳像素的选择基于等级的大小。相对于其他方法或“是/否”决策方法,这提供了大大改善的结果。将SPARC方法与代表各个季节(无雪夏季,有雪/冰覆盖的冬季和过渡季节)的许多AVHRR场景的监督分类结果进行了比较。结果表明,自动化(SPARC)和监督分类之间的总体协议水平为80%到91%。

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