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of Advanced Very High Resolution Radiometer (AVHRR) data over sediment-laden sea ice surfaces. In particular, the effects of solar elevation, viewing geometry, and atmospheric properties are considered. The atmospheric corrections are necessary for certain geometries and surface types. constraint of...
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.7146 http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/07HLEH.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.532.7146 2023-05-15T18:17:11+02:00 e d The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.7146 http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/07HLEH.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.7146 http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/07HLEH.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/07HLEH.pdf Sea ice Atmospheric correction Remote sensing text ftciteseerx 2016-01-08T10:41:07Z of Advanced Very High Resolution Radiometer (AVHRR) data over sediment-laden sea ice surfaces. In particular, the effects of solar elevation, viewing geometry, and atmospheric properties are considered. The atmospheric corrections are necessary for certain geometries and surface types. constraint of model simulations (Curry et al., 2001; Perovich, 1998; Robinson et al., 1992). This is particularly acute for large-scale estimates based on remotely-sensed data. While some of the key processes governing albedo evolution of summer sea Text Sea ice Unknown |
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Sea ice Atmospheric correction Remote sensing |
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Sea ice Atmospheric correction Remote sensing e d |
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Sea ice Atmospheric correction Remote sensing |
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of Advanced Very High Resolution Radiometer (AVHRR) data over sediment-laden sea ice surfaces. In particular, the effects of solar elevation, viewing geometry, and atmospheric properties are considered. The atmospheric corrections are necessary for certain geometries and surface types. constraint of model simulations (Curry et al., 2001; Perovich, 1998; Robinson et al., 1992). This is particularly acute for large-scale estimates based on remotely-sensed data. While some of the key processes governing albedo evolution of summer sea |
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The Pennsylvania State University CiteSeerX Archives |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.7146 http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/07HLEH.pdf |
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Sea ice |
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Sea ice |
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http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/07HLEH.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.532.7146 http://www2.gi.alaska.edu/snowice/sea-lake-ice/papers/07HLEH.pdf |
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