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Record #187389:
- #187389
Main publication details
MARC recordModeling the ocean circulation in the Bering Sea / Haoguo Hu, Jia Wang.
| Title: | Modeling the ocean circulation in the Bering Sea / Haoguo Hu, Jia Wang. |
| Author(s): | Hu, Haoguo. Wang, Jia. |
| Date: | 2008. |
| In: | Chinese Journal of Polar Science. (2008.), Vol. 19(2) (2008) |
| Abstract: | Presents simulations of circulation and tidal current in Bering Sea, using three-dimensional Princeton Ocean Model. Simulated circulation pattern in deep basin is relatively stable, cyclonic, and has little seasonal change. Bering Slope Current between 200-1,000 m isobaths is estimated to be 5 Sv in volume transport. Kamchatka Current is estimated to be 5 Sv in volume transport. Bering shelf circulations vary with season, driven mainly by wind. Features are consistent with historical estimates. |
| Notes: | Chinese Journal of Polar Science. Vol. 19(2) :193-211 (2008). In special issue Pacific Arctic Group (PAG) model-data fusion studies in Arctic Ocean and subpolar seas. |
| Keywords: | 519.673 -- Modelling. 551.46 -- Oceanography, physical. 551.465 -- Oceanography, dynamics. 551.465.5 -- Ocean currents. 551.466.7 -- Oceanography, tides. C -- Oceanography, hydrography and hydrology. (*3) -- Arctic regions. (*60) -- Arctic Ocean and adjacent waters. (*662) -- Bering Sea and Strait. |
| SPRI record no.: | 187389 |
LDR 01674naa#a2200000#a#4500 001 SPRI-187389 005 20231001141831.0 007 ta 008 231001s2008####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-187389 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aHu, Haoguo. 245 10 ‡aModeling the ocean circulation in the Bering Sea /‡cHaoguo Hu, Jia Wang. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2008. 300 ## ‡ap. 193-211 :‡bill., diags., maps. 500 ## ‡aChinese Journal of Polar Science. Vol. 19(2) :193-211 (2008). 500 ## ‡aIn special issue Pacific Arctic Group (PAG) model-data fusion studies in Arctic Ocean and subpolar seas. 520 3# ‡aPresents simulations of circulation and tidal current in Bering Sea, using three-dimensional Princeton Ocean Model. Simulated circulation pattern in deep basin is relatively stable, cyclonic, and has little seasonal change. Bering Slope Current between 200-1,000 m isobaths is estimated to be 5 Sv in volume transport. Kamchatka Current is estimated to be 5 Sv in volume transport. Bering shelf circulations vary with season, driven mainly by wind. Features are consistent with historical estimates. 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡a551.46 -- Oceanography, physical.‡2udc 650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc 650 07 ‡a551.465.5 -- Ocean currents.‡2udc 650 07 ‡a551.466.7 -- Oceanography, tides.‡2udc 650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*662) -- Bering Sea and Strait.‡2udc 700 1# ‡aWang, Jia. 773 0# ‡7nnas ‡tChinese Journal of Polar Science. ‡gVol. 19(2) (2008) ‡wSPRI-143545 916 ## ‡a2009/08/11 -- JW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231001 ‡bJW