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Record #126182:

A thermodynanic--dynamic snow sea-ice model / Josef M. Oberhuber, David M. Holland, Lawrence A. Mysak.

Title: A thermodynanic--dynamic snow sea-ice model / Josef M. Oberhuber, David M. Holland, Lawrence A. Mysak.
Author(s): Oberhuber, Josef M.
Holland, David M.
Mysak, Lawrence A.
Date: 1993.
Publisher: Berlin: Springer
In: Ice in the climate system. (1993.),
Abstract: Describes addition of snow model to existing coupled sea-ice model/global-ocean general circulation model (Oberhuber, Journal of Physical Oceanography, 1993, 23(5) :808-829). Prognostic equation for snow thickness is presented which is forced by snowfall, snowmelt, snow ageing, and flooding of sea ice. Additionally, total snow-ice heat content is computed. Simulations indicate asymmetric behaviour of model Arctic and Antarctic regions. In Antarctic, it is important to have snow cover to obtain reasonable sea-ice simulation, whereas snow cover is less important in Arctic; heat content there plays important role in sea-ice simulation.
Notes:

In: Ice in the climate system / W. Richard Peltier, ed.

Keywords: 551.58 -- Climatology.
551.583 -- Climatic changes.
551.588 -- Climate, effect of man and environment.
551.588.5 -- Climate, relationship with ice.
551.465.7 -- Oceanography, energy budget.
551.465 -- Oceanography, dynamics.
551.326.7 -- Sea ice.
551.578.46 -- Snow cover and snow patches.
519.673 -- Modelling.
E6 -- Glaciology: floating ice.
(*60) -- Arctic Ocean and adjacent waters.
(*80) -- Southern Ocean.
(*7) -- Antarctic regions.
SPRI record no.: 126182

MARCXML

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100 1# ‡aOberhuber, Josef M.
245 12 ‡aA thermodynanic--dynamic snow sea-ice model /‡cJosef M. Oberhuber, David M. Holland, Lawrence A. Mysak.
260 ## ‡aBerlin :‡bSpringer,‡c1993.
300 ## ‡ap. 653-673 :‡bdiags.
490 0# ‡aNATO ASI Series. Series I, Global environmental change ;‡v12
500 ## ‡aIn: Ice in the climate system / W. Richard Peltier, ed.
520 3# ‡aDescribes addition of snow model to existing coupled sea-ice model/global-ocean general circulation model (Oberhuber, Journal of Physical Oceanography, 1993, 23(5) :808-829). Prognostic equation for snow thickness is presented which is forced by snowfall, snowmelt, snow ageing, and flooding of sea ice. Additionally, total snow-ice heat content is computed. Simulations indicate asymmetric behaviour of model Arctic and Antarctic regions. In Antarctic, it is important to have snow cover to obtain reasonable sea-ice simulation, whereas snow cover is less important in Arctic; heat content there plays important role in sea-ice simulation.
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.588 -- Climate, effect of man and environment.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a551.465.7 -- Oceanography, energy budget.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*80) -- Southern Ocean.‡2udc
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
700 1# ‡aHolland, David M.
700 1# ‡aMysak, Lawrence A.
773 0# ‡7nnam ‡aW. Richard Peltier, ed. ‡tIce in the climate system. ‡dBerlin : Springer, 1993. ‡wSPRI-126141
917 ## ‡aUnenhanced record from Muscat, imported 2019
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