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Record #112499:

Interannual characteristics of an 80 km resolution diagnostic Arctic ice--ocean model / John E. Ries, William D. Hibler, III.

Title: Interannual characteristics of an 80 km resolution diagnostic Arctic ice--ocean model / John E. Ries, William D. Hibler, III.
Author(s): Ries, John E.
Hibler, William D.,
Date: 1991.
In: Annals of Glaciology. (1991.), Vol. 15 (1991)
Abstract: Points out drawbacks to seasonal simulations with large-scale coupled ice--ocean models in reproducing features of ice and ocean circulation of Arctic Ocean, and of Greenland and Norwegian seas. To address this, model is constructed and integrated over three-year period, and is driven by daily atmospheric forcing. To examine effects of topographic resolution and eddy viscosity on model, similar simulations were performed with 160 km resolution model. Results of simulations are compared with each other, with buoy drift in Arctic Basin, and with observed ice-edge variations. Discusses results, which indicate that problems remain in vertical resolution in shallow regions, in treating penetrative convection, and in simulation of inflow into Arctic Basin through Fram Strait.
Notes:

Annals of Glaciology. Vol. 15 :155-162 (1991).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.46 -- Oceanography, physical.
551.465.7 -- Oceanography, energy budget.
551.326.1 -- Floating ice, distribution and movement.
519.673 -- Modelling.
E6 -- Glaciology: floating ice.
(*60) -- Arctic Ocean and adjacent waters.
(*601) -- Arctic basin.
(*617) -- Greenland Sea and Fram Strait.
(*615) -- Norwegian Sea.
SPRI record no.: 112499

MARCXML

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100 1# ‡aRies, John E.
245 10 ‡aInterannual characteristics of an 80 km resolution diagnostic Arctic ice--ocean model /‡cJohn E. Ries, William D. Hibler, III.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 155-162 :‡bdiags., tables, maps.
500 ## ‡aAnnals of Glaciology. Vol. 15 :155-162 (1991).
520 3# ‡aPoints out drawbacks to seasonal simulations with large-scale coupled ice--ocean models in reproducing features of ice and ocean circulation of Arctic Ocean, and of Greenland and Norwegian seas. To address this, model is constructed and integrated over three-year period, and is driven by daily atmospheric forcing. To examine effects of topographic resolution and eddy viscosity on model, similar simulations were performed with 160 km resolution model. Results of simulations are compared with each other, with buoy drift in Arctic Basin, and with observed ice-edge variations. Discusses results, which indicate that problems remain in vertical resolution in shallow regions, in treating penetrative convection, and in simulation of inflow into Arctic Basin through Fram Strait.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465.7 -- Oceanography, energy budget.‡2udc
650 07 ‡a551.326.1 -- Floating ice, distribution and movement.‡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(*601) -- Arctic basin.‡2udc
651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc
651 #7 ‡a(*615) -- Norwegian Sea.‡2udc
700 1# ‡aHibler, William D.,‡cIII.
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 15 (1991) ‡wSPRI-60773
917 ## ‡aUnenhanced record from Muscat, imported 2019
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