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Record #112483:
- #112483
Main publication details
MARC recordOn 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 |
LDR 01763naa#a2200000#a#4500 001 SPRI-112483 005 20230328192345.0 007 ta 008 230328s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-112483 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aZhang, Jinlun. 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 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230328