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Record #128947:

A first try at identification of sea ice using the three beam scatterometer of ERS-1 / F. Gohin, Alain Cavanié.

Title: A first try at identification of sea ice using the three beam scatterometer of ERS-1 / F. Gohin, Alain Cavanié.
Author(s): Gohin, F.
Cavanié, Alain.
Date: 1994.
In: International Journal of Remote Sensing. (1994.), Vol. 15(6) (1994)
Abstract: Regional-scale behaviour of backscattering at C-band is investigated using data of AMI-WIND instrument during November 1991 over Arctic Ocean. Normalized radar cross-section appears as linear function of incidence angle, whose two parameters vary considerably between zones of first- and multi-year sea ice. Once slope parameters of AMI-WIND data have been determined, measured normalized radar cross-sections are corrected to bring them to single reference incidence angle. False-colour mapping of variable displays first- and multi-year sea-ice zones as determined previously from several passive microwave sensors (ESMR, SSM/I)
Notes:

International Journal of Remote Sensing. Vol. 15(6) :1221-1228 (1994).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.326.3 -- Floating ice, structure and surface features.
551.326.021 -- Floating ice, satellite sensing.
629.783 -- Satellites.
53.087.23 -- Remote sensing.
E3 -- Glaciology: instruments and methods.
(*60) -- Arctic Ocean and adjacent waters.
SPRI record no.: 128947

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100 1# ‡aGohin, F.
245 12 ‡aA first try at identification of sea ice using the three beam scatterometer of ERS-1 /‡cF. Gohin, Alain Cavanié.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1994.
300 ## ‡ap. 1221-1228 :‡bdiags., maps.
500 ## ‡aInternational Journal of Remote Sensing. Vol. 15(6) :1221-1228 (1994).
520 3# ‡aRegional-scale behaviour of backscattering at C-band is investigated using data of AMI-WIND instrument during November 1991 over Arctic Ocean. Normalized radar cross-section appears as linear function of incidence angle, whose two parameters vary considerably between zones of first- and multi-year sea ice. Once slope parameters of AMI-WIND data have been determined, measured normalized radar cross-sections are corrected to bring them to single reference incidence angle. False-colour mapping of variable displays first- and multi-year sea-ice zones as determined previously from several passive microwave sensors (ESMR, SSM/I)
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.326.3 -- Floating ice, structure and surface features.‡2udc
650 07 ‡a551.326.021 -- Floating ice, satellite sensing.‡2udc
650 07 ‡a629.783 -- Satellites.‡2udc
650 07 ‡a53.087.23 -- Remote sensing.‡2udc
650 07 ‡aE3 -- Glaciology: instruments and methods.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
700 1# ‡aCavanié, Alain.
773 0# ‡7nnas ‡tInternational Journal of Remote Sensing. ‡gVol. 15(6) (1994) ‡wSPRI-1038
917 ## ‡aUnenhanced record from Muscat, imported 2019
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