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Record #200832:

Turbulent kinetic energy dissipation in Barrow Canyon / E.L. Shroyer.

Title: Turbulent kinetic energy dissipation in Barrow Canyon / E.L. Shroyer.
Author(s): Shroyer, E. L.
Date: 2012.
In: Journal of Physical Oceanography. (2012.), Vol. 42(6) (2012)
Abstract: Describes flow of Pacific Water (PW) across shallow Chukchi Sea before reaching Arctic Ocean. Substantial portion of PW is routed through Barrow Canyon, region of complex geometry and forcing, where various water masses have been observed to coexist. These factors contribute to dynamic physical environment, with potential for significant water mass transformation. Measurements of turbulent kinetic energy dissipation indicate that diapycnal mixing is important in upper canyon.
Notes:

Journal of Physical Oceanography. Vol. 42(6) :1012-1021 (2012).

Keywords: 551.46 -- Oceanography, physical.
551.462.34 -- Submarine canyons.
551.465 -- Oceanography, dynamics.
551.465.4 -- Oceanography, stratification.
551.465.45 -- Water masses.
C -- Oceanography, hydrography and hydrology.
(*3) -- Arctic regions.
(*60) -- Arctic Ocean and adjacent waters.
(*628.2) -- Alaskan Beaufort Sea.
(*661) -- Alaskan waters.
(*682) -- Chukchi Sea.
SPRI record no.: 200832

MARCXML

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001 SPRI-200832
005 20221004211612.0
007 ta
008 221004s2012####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-200832
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aShroyer, E. L.
245 10 ‡aTurbulent kinetic energy dissipation in Barrow Canyon /‡cE.L. Shroyer.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2012.
300 ## ‡ap. 1012-1021 :‡bill. (some col.), diags., table, map.
500 ## ‡aJournal of Physical Oceanography. Vol. 42(6) :1012-1021 (2012).
520 3# ‡aDescribes flow of Pacific Water (PW) across shallow Chukchi Sea before reaching Arctic Ocean. Substantial portion of PW is routed through Barrow Canyon, region of complex geometry and forcing, where various water masses have been observed to coexist. These factors contribute to dynamic physical environment, with potential for significant water mass transformation. Measurements of turbulent kinetic energy dissipation indicate that diapycnal mixing is important in upper canyon.
530 ## ‡aAlso issued online ‡uurn:doi:10.1175/JPO-D-11-0184.1‡uhttps://dx.doi.org/10.1175/JPO-D-11-0184.1
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.462.34 -- Submarine canyons.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.465.4 -- Oceanography, stratification.‡2udc
650 07 ‡a551.465.45 -- Water masses.‡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(*628.2) -- Alaskan Beaufort Sea.‡2udc
651 #7 ‡a(*661) -- Alaskan waters.‡2udc
651 #7 ‡a(*682) -- Chukchi Sea.‡2udc
773 0# ‡7nnas ‡tJournal of Physical Oceanography. ‡gVol. 42(6) (2012) ‡wSPRI-78712
916 ## ‡a2012/10/04 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221004 ‡bJW