Detecting Arctic snow and ice cover with FY-1D global data
Chinese meteorological satellite FY-1D can obtain global data from four spectral channels which include visible channel (0.58 - 0.68 µm) and infrared channels (0.84 - 0.89 µm, 10.3 - 11.3 µm, 11.5 - 12.5 µm). 2366 snow and ice samples, 2024 cloud samples, 1602 land samples and 1648 water samples wer...
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Polar Research Institute of China - PRIC
2007
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Online Access: | http://library.arcticportal.org/2331/ http://library.arcticportal.org/2331/1/A200701007.pdf |
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ftarcticportal:oai:generic.eprints.org:2331 2023-10-01T03:49:45+02:00 Detecting Arctic snow and ice cover with FY-1D global data Xiaoping, Xie Yujie, Liu Bingyu, Du 2007-06 application/pdf http://library.arcticportal.org/2331/ http://library.arcticportal.org/2331/1/A200701007.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2331/1/A200701007.pdf Xiaoping, Xie and Yujie, Liu and Bingyu, Du (2007) Detecting Arctic snow and ice cover with FY-1D global data. Advances in Polar Science, 18 (1). pp. 54-62. Cryosphere Article PeerReviewed 2007 ftarcticportal 2023-09-06T22:54:10Z Chinese meteorological satellite FY-1D can obtain global data from four spectral channels which include visible channel (0.58 - 0.68 µm) and infrared channels (0.84 - 0.89 µm, 10.3 - 11.3 µm, 11.5 - 12.5 µm). 2366 snow and ice samples, 2024 cloud samples, 1602 land samples and 1648 water samples were selected randomly from Arctic imageries. Land and water can be detected by spectral features Snow-ice and cloud can be classified by textural features. The classifier is Bayes classifier. By synthesizing five days classifying result of Arctic snow and ice cover area, complete Arctic snow and ice cover area can be obtained. The result agrees with NO-AA/NESD IS MS products up to 70%. Article in Journal/Newspaper Advances in Polar Science Arctic Arctic Polar Science Polar Science Arctic Portal Library Arctic |
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Open Polar |
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Arctic Portal Library |
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ftarcticportal |
language |
English |
topic |
Cryosphere |
spellingShingle |
Cryosphere Xiaoping, Xie Yujie, Liu Bingyu, Du Detecting Arctic snow and ice cover with FY-1D global data |
topic_facet |
Cryosphere |
description |
Chinese meteorological satellite FY-1D can obtain global data from four spectral channels which include visible channel (0.58 - 0.68 µm) and infrared channels (0.84 - 0.89 µm, 10.3 - 11.3 µm, 11.5 - 12.5 µm). 2366 snow and ice samples, 2024 cloud samples, 1602 land samples and 1648 water samples were selected randomly from Arctic imageries. Land and water can be detected by spectral features Snow-ice and cloud can be classified by textural features. The classifier is Bayes classifier. By synthesizing five days classifying result of Arctic snow and ice cover area, complete Arctic snow and ice cover area can be obtained. The result agrees with NO-AA/NESD IS MS products up to 70%. |
format |
Article in Journal/Newspaper |
author |
Xiaoping, Xie Yujie, Liu Bingyu, Du |
author_facet |
Xiaoping, Xie Yujie, Liu Bingyu, Du |
author_sort |
Xiaoping, Xie |
title |
Detecting Arctic snow and ice cover with FY-1D global data |
title_short |
Detecting Arctic snow and ice cover with FY-1D global data |
title_full |
Detecting Arctic snow and ice cover with FY-1D global data |
title_fullStr |
Detecting Arctic snow and ice cover with FY-1D global data |
title_full_unstemmed |
Detecting Arctic snow and ice cover with FY-1D global data |
title_sort |
detecting arctic snow and ice cover with fy-1d global data |
publisher |
Polar Research Institute of China - PRIC |
publishDate |
2007 |
url |
http://library.arcticportal.org/2331/ http://library.arcticportal.org/2331/1/A200701007.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Advances in Polar Science Arctic Arctic Polar Science Polar Science |
genre_facet |
Advances in Polar Science Arctic Arctic Polar Science Polar Science |
op_relation |
http://library.arcticportal.org/2331/1/A200701007.pdf Xiaoping, Xie and Yujie, Liu and Bingyu, Du (2007) Detecting Arctic snow and ice cover with FY-1D global data. Advances in Polar Science, 18 (1). pp. 54-62. |
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1778528648334147584 |