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Record #112803:

A comparison of sea ice parameters computed from advanced very high resolution radiometer and Landsat satellite imagery and from airborne passive microwave radiometry / W.J. Emery, M. Radebaugh, C.W. Fowler, Donald J. Cavalieri, Konrad Steffen.

Title: A comparison of sea ice parameters computed from advanced very high resolution radiometer and Landsat satellite imagery and from airborne passive microwave radiometry / W.J. Emery, M. Radebaugh, C.W. Fowler, Donald J. Cavalieri, Konrad Steffen.
Author(s): Emery, W. J.
Radebaugh, M.
Fowler, C. W.
Cavalieri, Donald J.
Steffen, Konrad.
Date: 1991.
In: Journal of Geophysical Research. (1991.), Vol. 96(C12) (1991)
Abstract: Comparisons suggest that near-infrared (channel 2) AVHRR imagery can be used to compute ice concentrations within ±7 to 18% (rms differences) and ice-edge locations accurate to ±3 to 4 km (rms differences). Ice parameters computed from thermal infrared (channel 4) AVHRR imagery are less accurate. Appears reasonable to conclude that AVHRR ice concentration calculation is accurate to about ±10% with channel 2 and ±15% with channel 4. Errors in Landsat ice concentrations are estimated to be within 2 to 3% after corrections.
Notes:

Journal of Geophysical Research. Vol. 96(C12) :22, 075-22, 085 (1991).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.326.021 -- Floating ice, satellite sensing.
551.326.022 -- Floating ice, airborne sensing.
629.783 -- Satellites.
53.087.23 -- Remote sensing.
519.673 -- Modelling.
551.326.12 -- Floating ice, distribution, seasonal.
E6 -- Glaciology: floating ice.
SPRI record no.: 112803

MARCXML

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245 02 ‡aA comparison of sea ice parameters computed from advanced very high resolution radiometer and Landsat satellite imagery and from airborne passive microwave radiometry /‡cW.J. Emery, M. Radebaugh, C.W. Fowler, Donald J. Cavalieri, Konrad Steffen.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 22, 075-22, 085 :‡bill., diags., tables, map.
500 ## ‡aJournal of Geophysical Research. Vol. 96(C12) :22, 075-22, 085 (1991).
520 3# ‡aComparisons suggest that near-infrared (channel 2) AVHRR imagery can be used to compute ice concentrations within ±7 to 18% (rms differences) and ice-edge locations accurate to ±3 to 4 km (rms differences). Ice parameters computed from thermal infrared (channel 4) AVHRR imagery are less accurate. Appears reasonable to conclude that AVHRR ice concentration calculation is accurate to about ±10% with channel 2 and ±15% with channel 4. Errors in Landsat ice concentrations are estimated to be within 2 to 3% after corrections.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.326.021 -- Floating ice, satellite sensing.‡2udc
650 07 ‡a551.326.022 -- Floating ice, airborne sensing.‡2udc
650 07 ‡a629.783 -- Satellites.‡2udc
650 07 ‡a53.087.23 -- Remote sensing.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a551.326.12 -- Floating ice, distribution, seasonal.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
700 1# ‡aEmery, W. J.
700 1# ‡aRadebaugh, M.
700 1# ‡aFowler, C. W.
700 1# ‡aCavalieri, Donald J.
700 1# ‡aSteffen, Konrad.
773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 96(C12) (1991) ‡wSPRI-35252
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240305