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Record #189102:

Pacific water transport in the western Arctic Ocean simulated by an eddy-resolving coupled sea ice-ocean model / Eiji Watanabe, Hiroyasu Hasumi.

Title: Pacific water transport in the western Arctic Ocean simulated by an eddy-resolving coupled sea ice-ocean model / Eiji Watanabe, Hiroyasu Hasumi.
Author(s): Watanabe, Eiji.
Hasumi, Hiroyasu.
Date: 2009.
In: Journal of Physical Oceanography. (2009.), Vol. 39(9) (2009)
Abstract: Investigates process of Pacific water transport in Chukchi Sea and southern Canada Basin using eddy-resolving coupled sea ice-ocean model. Simulation result demonstrates that Pacific water flows into basin by mesoscale baroclinic eddies, which are generated and developed as result of instability of narrow and intense jet through Barrow Canyon. Each eddy has baroclinic anticyclonic structure, and its horizontal and vertical scales grow as result of merging with others during August and September.
Notes:

Journal of Physical Oceanography. Vol. 39(9) :2, 194-2, 211 (2009).

Keywords: 519.673 -- Modelling.
551.326.7 -- Sea ice.
551.46 -- Oceanography, physical.
551.463.6 -- Sea water, thermal properties and heat flux.
551.465 -- Oceanography, dynamics.
551.465.7 -- Oceanography, energy budget.
C -- Oceanography, hydrography and hydrology.
(*3) -- Arctic regions.
(*628) -- Beaufort Sea.
(*66) -- North Pacific Ocean.
(*682) -- Chukchi Sea.
SPRI record no.: 189102

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245 10 ‡aPacific water transport in the western Arctic Ocean simulated by an eddy-resolving coupled sea ice-ocean model /‡cEiji Watanabe, Hiroyasu Hasumi.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2009.
300 ## ‡ap. 2, 194-2, 211 :‡bill., diags., maps.
500 ## ‡aJournal of Physical Oceanography. Vol. 39(9) :2, 194-2, 211 (2009).
520 3# ‡aInvestigates process of Pacific water transport in Chukchi Sea and southern Canada Basin using eddy-resolving coupled sea ice-ocean model. Simulation result demonstrates that Pacific water flows into basin by mesoscale baroclinic eddies, which are generated and developed as result of instability of narrow and intense jet through Barrow Canyon. Each eddy has baroclinic anticyclonic structure, and its horizontal and vertical scales grow as result of merging with others during August and September.
530 ## ‡aAlso issued online ‡uurn:doi:10.1175/2009JPO4010.1‡uhttps://dx.doi.org/10.1175/2009JPO4010.1
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.463.6 -- Sea water, thermal properties and heat flux.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.465.7 -- Oceanography, energy budget.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*628) -- Beaufort Sea.‡2udc
651 #7 ‡a(*66) -- North Pacific Ocean.‡2udc
651 #7 ‡a(*682) -- Chukchi Sea.‡2udc
700 1# ‡aHasumi, Hiroyasu.
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