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Record #112483:

On the role of ocean circulation in seasonal and interannual ice-edge variations in the Bering Sea / Jinlun Zhang, William D. Hibler, III.

Title: On the role of ocean circulation in seasonal and interannual ice-edge variations in the Bering Sea / Jinlun Zhang, William D. Hibler, III.
Author(s): Zhang, Jinlun.
Hibler, William D.,
Date: 1991.
In: Annals of Glaciology. (1991.), Vol. 15 (1991)
Abstract: 40 km-resolution ice-ocean model was used to investigate effects of ocean circulation and vertical convection on these variations. Results were not totally satisfactory: coupled ice-ocean model gave significantly better results than ice-only model for ice margin, but ocean currents over shelf and shelf break were not realistic. Winter average ice-velocity distributions do, however, appear reasonable and consistent with winds. Results suggest that enhanced vertical resolution, with more complete boundary-layer formulation, will be required to achieve realistic seasonal simulations of system.
Notes:

Annals of Glaciology. Vol. 15 :37-44 (1991).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
519.673 -- Modelling.
551.326.1 -- Floating ice, distribution and movement.
551.46 -- Oceanography, physical.
551.465 -- Oceanography, dynamics.
551.465.7 -- Oceanography, energy budget.
E6 -- Glaciology: floating ice.
(*60) -- Arctic Ocean and adjacent waters.
(*662) -- Bering Sea and Strait.
SPRI record no.: 112483

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245 10 ‡aOn the role of ocean circulation in seasonal and interannual ice-edge variations in the Bering Sea /‡cJinlun Zhang, William D. Hibler, III.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 37-44 :‡bdiags., maps.
500 ## ‡aAnnals of Glaciology. Vol. 15 :37-44 (1991).
520 3# ‡a40 km-resolution ice-ocean model was used to investigate effects of ocean circulation and vertical convection on these variations. Results were not totally satisfactory: coupled ice-ocean model gave significantly better results than ice-only model for ice margin, but ocean currents over shelf and shelf break were not realistic. Winter average ice-velocity distributions do, however, appear reasonable and consistent with winds. Results suggest that enhanced vertical resolution, with more complete boundary-layer formulation, will be required to achieve realistic seasonal simulations of system.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a551.326.1 -- Floating ice, distribution and movement.‡2udc
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.465.7 -- Oceanography, energy budget.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*662) -- Bering Sea and Strait.‡2udc
700 1# ‡aHibler, William D.,‡cIII.
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 15 (1991) ‡wSPRI-60773
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