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Record #119652:

Sea ice thickness distributions derived from archived aerial photographs of the Arctic sea ice pack / D.T. Eppler, L.D. Farmer.

Title: Sea ice thickness distributions derived from archived aerial photographs of the Arctic sea ice pack / D.T. Eppler, L.D. Farmer.
Author(s): Eppler, D. T.
Farmer, L. D.
Date: 1992.
Publisher: Seattle, WA: University of Washington, Applied Physics Laboratory, Polar Science Center
In: Report of the Sea Ice Thickness Workshop, 19-21 November 1991, New Carrollton, Maryland. (1992.),
Abstract: Gray tones that characterize new and young sea ice in air photographs vary as function of ice thickness because albedo, reflectivity, scattering and absorption of ice at optical wavelengths depend on thickness. This fact permits thickness distribution of thinner ice types (<30 cm) to be derived from black-and-white photographs, yielding excellent source of information about sea-ice thickness distribution in 0 to 30 cm range.
Notes:

In: Report of the Sea Ice Thickness Workshop, 19-21 November 1991, New Carrollton, Maryland / Alan S. Thorndike, Claire L. Parkinson, D.A. Rothrock, eds.

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.326.3 -- Floating ice, structure and surface features.
551.326.022 -- Floating ice, airborne sensing.
551.321.6 -- Ice thickness, measurement.
528.77 -- Air photographs.
53.087.23 -- Remote sensing.
E3 -- Glaciology: instruments and methods.
(*60) -- Arctic Ocean and adjacent waters.
SPRI record no.: 119652

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100 1# ‡aEppler, D. T.
245 10 ‡aSea ice thickness distributions derived from archived aerial photographs of the Arctic sea ice pack /‡cD.T. Eppler, L.D. Farmer.
260 ## ‡aSeattle, WA :‡bUniversity of Washington, Applied Physics Laboratory, Polar Science Center,‡c1992.
300 ## ‡ap. B10-B15 :‡btables, map.
500 ## ‡aIn: Report of the Sea Ice Thickness Workshop, 19-21 November 1991, New Carrollton, Maryland / Alan S. Thorndike, Claire L. Parkinson, D.A. Rothrock, eds.
520 3# ‡aGray tones that characterize new and young sea ice in air photographs vary as function of ice thickness because albedo, reflectivity, scattering and absorption of ice at optical wavelengths depend on thickness. This fact permits thickness distribution of thinner ice types (<30 cm) to be derived from black-and-white photographs, yielding excellent source of information about sea-ice thickness distribution in 0 to 30 cm range.
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 ‡a551.326.022 -- Floating ice, airborne sensing.‡2udc
650 07 ‡a551.321.6 -- Ice thickness, measurement.‡2udc
650 07 ‡a528.77 -- Air photographs.‡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# ‡aFarmer, L. D.
773 0# ‡7nnam ‡aAlan S. Thorndike, Claire L. Parkinson, D.A. Rothrock, eds. ‡tReport of the Sea Ice Thickness Workshop, 19-21 November 1991, New Carrollton, Maryland. ‡dSeattle, WA : University of Washington, Applied Physics Laboratory, Polar Science Center, 1992. ‡wSPRI-119645
917 ## ‡aUnenhanced record from Muscat, imported 2019
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