High-latitude surface temperature estimates from thermal satellite data
The surface temperature of the polar regions controls sea ice growth, snow melt, and surface-atmosphere energy exchange. However, our limited knowledge of polar surfaces and atmospheres has hampered the development of methods to estimate surface temperature with satellite data. In this article, clea...
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Veröffentlicht in: | Remote sensing of environment 1997-08, Vol.61 (2), p.302-309 |
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creator | Key, Jeffrey R. Collins, John B. Fowler, Charles Stone, Robert S. |
description | The surface temperature of the polar regions controls sea ice growth, snow melt, and surface-atmosphere energy exchange. However, our limited knowledge of polar surfaces and atmospheres has hampered the development of methods to estimate surface temperature with satellite data. In this article, clear-sky surface-temperature retrieval algorithms for rise with the Advanced Very High Resolution Radiometer (AVHRR) and the Along Track Scanning Radiometer (ATSR) for the Arctic and the Antarctic, over ocean and land, are presented. The methods are similar to those used in estimating sea and land surface temperatures but are developed with. data specific to the polar regions. An extensive validation analysis using an annual cycle of .surface meamarements gives accuracies in the range of 0.3–2.1 K, the larger errors being attributable to the spatially variable .surface of the validation area. For homogeneous surfaces the expected accuracy is sufficient for many climate process studies. |
doi_str_mv | 10.1016/S0034-4257(97)89497-7 |
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However, our limited knowledge of polar surfaces and atmospheres has hampered the development of methods to estimate surface temperature with satellite data. In this article, clear-sky surface-temperature retrieval algorithms for rise with the Advanced Very High Resolution Radiometer (AVHRR) and the Along Track Scanning Radiometer (ATSR) for the Arctic and the Antarctic, over ocean and land, are presented. The methods are similar to those used in estimating sea and land surface temperatures but are developed with. data specific to the polar regions. An extensive validation analysis using an annual cycle of .surface meamarements gives accuracies in the range of 0.3–2.1 K, the larger errors being attributable to the spatially variable .surface of the validation area. 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However, our limited knowledge of polar surfaces and atmospheres has hampered the development of methods to estimate surface temperature with satellite data. In this article, clear-sky surface-temperature retrieval algorithms for rise with the Advanced Very High Resolution Radiometer (AVHRR) and the Along Track Scanning Radiometer (ATSR) for the Arctic and the Antarctic, over ocean and land, are presented. The methods are similar to those used in estimating sea and land surface temperatures but are developed with. data specific to the polar regions. An extensive validation analysis using an annual cycle of .surface meamarements gives accuracies in the range of 0.3–2.1 K, the larger errors being attributable to the spatially variable .surface of the validation area. For homogeneous surfaces the expected accuracy is sufficient for many climate process studies.</description><subject>Algorithms</subject><subject>Earth, ocean, space</subject><subject>Errors</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Geophysics. 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subjects | Algorithms Earth, ocean, space Errors Exact sciences and technology External geophysics Geophysics. Techniques, methods, instrumentation and models Parameter estimation Radiometers Remote sensing Surfaces Weather satellites |
title | High-latitude surface temperature estimates from thermal satellite data |
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