Comparison of sea ice signatures in OKEAN and RADARSAT radar images for the northeastern Barents Sea
Sea ice signatures in near-simultaneous OKEAN real aperture radar (RAR) and RADARSAT synthetic aperture radar (ScanSAR) images have been analyzed and compared for the northeastern part of the Barents Sea in April 1998. Signatures of major sea ice types and features in these images have been identifi...
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Published in | Canadian journal of remote sensing Vol. 30; no. 6; pp. 882 - 892 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
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Taylor & Francis
01.12.2004
Canadian Aeronautics and Space Institute |
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Abstract | Sea ice signatures in near-simultaneous OKEAN real aperture radar (RAR) and RADARSAT synthetic aperture radar (ScanSAR) images have been analyzed and compared for the northeastern part of the Barents Sea in April 1998. Signatures of major sea ice types and features in these images have been identified and verified by in situ observations on board the nuclear icebreaker Sovetsky Soyuz. It is shown that both RAR and ScanSAR images can be used for detection of new, young, first year, and multiyear sea ice types, multiyear and fast ice boundaries, flaw polynyas, wide fractures, giant and vast ice floes, and large areas of rough ice. Backscatter signatures of the major sea ice types are analyzed and compared, and the backscattering differences between the ice types are estimated for both types of data. High-resolution ScanSAR images are found to be particularly suited for discrimination of narrow leads and level areas in compact sea ice. A study of the radar signatures of a flaw polynya to the north of Cape Zhelaniya was conducted using ERS SAR, RADARSAT ScanSAR, and OKEAN RAR over a period of 33 h. The backscatter from the polynya varied significantly between VV and HH polarization and as a consequence of changing physical properties due to freezing during the 33 h period. Access to satellite radar data for use in sea ice research will increase in the near future. Wide-swath SAR data are available from both RADARSAT and ENVISAT from 2003, and a new RAR satellite, SICH-M1, is planned for launch in 2004. |
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AbstractList | Sea ice signatures in near-simultaneous OKEAN real aperture radar (RAR) and RADARSAT synthetic aperture radar (ScanSAR) images have been analyzed and compared for the northeastern part of the Barents Sea in April 1998. Signatures of major sea ice types and features in these images have been identified and verified by in situ observations on board the nuclear icebreaker Sovetsky Soyuz. It is shown that both RAR and ScanSAR images can be used for detection of new, young, first year, and multiyear sea ice types, multiyear and fast ice boundaries, flaw polynyas, wide fractures, giant and vast ice floes, and large areas of rough ice. Backscatter signatures of the major sea ice types are analyzed and compared, and the backscattering differences between the ice types are estimated for both types of data. High-resolution ScanSAR images are found to be particularly suited for discrimination of narrow leads and level areas in compact sea ice. A study of the radar signatures of a flaw polynya to the north of Cape Zhelaniya was conducted using ERS SAR, RADARSAT ScanSAR, and OKEAN RAR over a period of 33 h. The backscatter from the polynya varied significantly between VV and HH polarization and as a consequence of changing physical properties due to freezing during the 33 h period. Access to satellite radar data for use in sea ice research will increase in the near future. Wide-swath SAR data are available from both RADARSAT and ENVISAT from 2003, and a new RAR satellite, SICH-M1, is planned for launch in 2004.Original Abstract: Dans cette etude, les signatures de la glace de mer dans les images quasi-simultanees radar a antenne reelle (RAR) de OKEAN et ScanRAR a synthese d'ouverture de RADARSAT ont ete analysees et comparees pour la region du nord-est de la mer de Barents, en avril 1998. Les signatures des principaux types de glace de mer et leurs caracteristiques observees dans ces images ont etes identifiees et verifiees par des observations in situ realisees a partir du brise-glace nucleaire Sovetsky Soyuz. Il est demontre qu'autant les images RAR que les images ScanSAR peuvent etre utilisees pour la detection des types de glace nouvelle, jeune ou datant d'une ou de plusieurs annees, des limites de la banquise compacte, des'polynies de separation, des grandes fractures, des icebergs geants et des grandes zones de glace rugueuse. Les signatures de la retrodiffusion des principaux types de glace sont analysees et comparees, et les differences dans la retrodiffusion sont estimees pour les deux types de donnees. Il a ete possible d'observer que les images ScanSAR a haute resolution sont particulierement bien adaptees a la detection des chenaux etroits et des surfaces planes dans les zones de glace de mer compacte. Une etude des signatures radar des polynies de separation au nord du Cap Zhelaniya a ete realisee en utilisant les donnees RSO de ERS, ScanSAR de RADARSAT et RAR de Okean sur une periode de 33 h. La retrodiffusion provenant des polynies varie significativement entre la polarisation VV et HH et en raison des proprietes physiques changeantes enregistrees lors d'une periode de gel. L'acces aux donnees satellite radar a des fins de recherche sur la glace devrait etre facilite dans un avenir prochain. Depuis 2003, des donnees RSO a faisceau large sont disponibles a partir de RADARSAT et ENVISAT, alors que le lancement d'un nouveau satellite RAR, le satellite SICH-M1, est prevu pour 2004. [Traduit par la Redaction] Sea ice signatures in near-simultaneous OKEAN real aperture radar (RAR) and RADARSAT synthetic aperture radar (ScanSAR) images have been analyzed and compared for the northeastern part of the Barents Sea in April 1998. Signatures of major sea ice types and features in these images have been identified and verified by in situ observations on board the nuclear icebreaker Sovetsky Soyuz. It is shown that both RAR and ScanSAR images can be used for detection of new, young, first year, and multiyear sea ice types, multiyear and fast ice boundaries, flaw polynyas, wide fractures, giant and vast ice floes, and large areas of rough ice. Backscatter signatures of the major sea ice types are analyzed and compared, and the backscattering differences between the ice types are estimated for both types of data. High-resolution ScanSAR images are found to be particularly suited for discrimination of narrow leads and level areas in compact sea ice. A study of the radar signatures of a flaw polynya to the north of Cape Zhelaniya was conducted using ERS SAR, RADARSAT ScanSAR, and OKEAN RAR over a period of 33 h. The backscatter from the polynya varied significantly between VV and HH polarization and as a consequence of changing physical properties due to freezing during the 33 h period. Access to satellite radar data for use in sea ice research will increase in the near future. Wide-swath SAR data are available from both RADARSAT and ENVISAT from 2003, and a new RAR satellite, SICH-M1, is planned for launch in 2004. |
Author | Sandven, S. Bobylev, L P Alexandrov, V Y Kloster, K. Zaitsev, L V |
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References | Johannessen O.M. (p_59) 2004; 56 Alexandrov V.Y. (p_48) 2000; 36 Drinkwater M.R. (p_54) 1992; 68 Ulander L.M.H. (p_77) 1997; 16 Bushuev A.V. (p_53) 1995; 70 Emery W.J. (p_55) 1997; 24 Sandven S. (p_74) 1999; 104 Loeng H. (p_63) 1979; 2 Onstott R.G. (p_68) 1992; 68 Zakharov V.F. (p_82) 1976; 337 Nghiem S.V. (p_67) 1997; 102 Krovotyntsev V.A. (p_61) 2000; 16 Pfirman S.L. (p_69) 1997; 102 Falck-Petersen S. (p_56) 2000; 27 Johannessen O.M. (p_58) 2000; 16 Vinje T. (p_80) 1990; 10 Sandven S. (p_75) 2001; 27 Volkov A.M. (p_81) 1995; 13 Sandven S. (p_73) 1993; 13 Rignot E. (p_72) 1994; 40 Alexandrov V.Y. (p_47) 2000; 105 Melling H. (p_65) 1998; 19 Beaven S.G. (p_49) 1994; 15 Martin T. (p_64) 2000; 105 Kwok R. (p_62) 2002; 107 Belchanskii G.I. (p_50) 2001; 16 |
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Title | Comparison of sea ice signatures in OKEAN and RADARSAT radar images for the northeastern Barents Sea |
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