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Record #145546:

The possible effects of including ridge-related roughness in air--ice drag parameterization: a sensitivity study / L.-B. Tremblay, Lawrence A. Mysak.

Title: The possible effects of including ridge-related roughness in air--ice drag parameterization: a sensitivity study / L.-B. Tremblay, Lawrence A. Mysak.
Author(s): Tremblay, L. -B.
Mysak, Lawrence A.
Date: 1997.
In: Annals of Glaciology. (1997.), Vol. 25 (1997)
Abstract: Includes ridge-related roughness in drag parameterization of effects on ice-thickness distribution, using sea-ice dynamic and thermodynamic model. Incorporates winds and ocean currents in construction of climatological thickness fields. Compared to constant drag cofficient model, results that include roughness have significantly different spatial distribution, with much thicker ice in western Arctic, and match observations better.
Notes:

Annals of Glaciology. Vol. 25 :22-25 (1997)

Papers from the International Symposium on Representation of the Cryosphere in Climate and Hydrological Models, 12--15 August 1996, Victoria, B.C., Canada, J.E. Walsh (Editor)

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
536 -- Heat.
551.326.37 -- Pressure ridges.
551.326.7 -- Sea ice.
551.58 -- Climatology.
551.588.5 -- Climate, relationship with ice.
551.46 -- Oceanography, physical.
551.465.5 -- Ocean currents.
551.5 -- Meteorology.
551.556 -- Wind, effects of.
519.673 -- Modelling.
E6 -- Glaciology: floating ice.
(*60) -- Arctic Ocean and adjacent waters.
SPRI record no.: 145546

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245 14 ‡aThe possible effects of including ridge-related roughness in air--ice drag parameterization :‡ba sensitivity study /‡cL.-B. Tremblay, Lawrence A. Mysak.
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500 ## ‡aAnnals of Glaciology. Vol. 25 :22-25 (1997)
500 ## ‡aPapers from the International Symposium on Representation of the Cryosphere in Climate and Hydrological Models, 12--15 August 1996, Victoria, B.C., Canada, J.E. Walsh (Editor)
520 3# ‡aIncludes ridge-related roughness in drag parameterization of effects on ice-thickness distribution, using sea-ice dynamic and thermodynamic model. Incorporates winds and ocean currents in construction of climatological thickness fields. Compared to constant drag cofficient model, results that include roughness have significantly different spatial distribution, with much thicker ice in western Arctic, and match observations better.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a536 -- Heat.‡2udc
650 07 ‡a551.326.37 -- Pressure ridges.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465.5 -- Ocean currents.‡2udc
650 07 ‡a551.5 -- Meteorology.‡2udc
650 07 ‡a551.556 -- Wind, effects of.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
700 1# ‡aMysak, Lawrence A.
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 25 (1997) ‡wSPRI-60773
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