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Record #207037:

Vertical heat transport by ocean circulation and the role of mechanical and haline forcing / Jan D. Zika, Willem P. Sijp, Matthew H. England.

Title: Vertical heat transport by ocean circulation and the role of mechanical and haline forcing / Jan D. Zika, Willem P. Sijp, Matthew H. England.
Author(s): Zika, Jan D.
Sijp, Willem P.
England, Matthew H.
Date: 2013.
In: Journal of Physical Oceanography. (2013.), Vol. 43(10) (2013)
Abstract: Investigates vertical transport of heat by ocean circulation using coupled climate model and novel thermodynamic methods. Identifies three cells in model: thermally direct (flux heat upward) cell coincident with Antarctic Bottom Water; thermally indirect (flux heat downward) deep cell coincident with upper limb of meridional overturning circulation; and thermally direct shallow cell coincident with subtropical gyres at surface.
Notes:

Journal of Physical Oceanography. Vol. 43(10) :2095-2112 (2013).

Keywords: 551.46 -- Oceanography, physical.
551.465 -- Oceanography, dynamics.
551.465.45 -- Water masses.
551.465.5 -- Ocean currents.
551.464 -- Sea water, chemical properties.
551.464.5 -- Salinity.
551.463 -- Sea water, physical properties.
551.463.6 -- Sea water, thermal properties and heat flux.
551.5 -- Meteorology.
551.55 -- Wind and air turbulence.
519.673 -- Modelling.
C -- Oceanography, hydrography and hydrology.
(*7) -- Antarctic regions.
(*80) -- Southern Ocean.
(*86) -- Southern Ocean, Australian sector.
SPRI record no.: 207037

MARCXML

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001 SPRI-207037
005 20220928182606.0
007 ta
008 220928s2013####xx#a##|##|###|0||#0|eng#d
035 ## ‡aSPRI-207037
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aZika, Jan D.
245 10 ‡aVertical heat transport by ocean circulation and the role of mechanical and haline forcing /‡cJan D. Zika, Willem P. Sijp, Matthew H. England.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2013.
300 ## ‡ap. 2095-2112 :‡bill., diags.
500 ## ‡aJournal of Physical Oceanography. Vol. 43(10) :2095-2112 (2013).
520 3# ‡aInvestigates vertical transport of heat by ocean circulation using coupled climate model and novel thermodynamic methods. Identifies three cells in model: thermally direct (flux heat upward) cell coincident with Antarctic Bottom Water; thermally indirect (flux heat downward) deep cell coincident with upper limb of meridional overturning circulation; and thermally direct shallow cell coincident with subtropical gyres at surface.
530 ## ‡aAlso issued online ‡uurn:doi:10.1175/JPO-D-12-0179.1‡uhttps://dx.doi.org/10.1175/JPO-D-12-0179.1
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.465.45 -- Water masses.‡2udc
650 07 ‡a551.465.5 -- Ocean currents.‡2udc
650 07 ‡a551.464 -- Sea water, chemical properties.‡2udc
650 07 ‡a551.464.5 -- Salinity.‡2udc
650 07 ‡a551.463 -- Sea water, physical properties.‡2udc
650 07 ‡a551.463.6 -- Sea water, thermal properties and heat flux.‡2udc
650 07 ‡a551.5 -- Meteorology.‡2udc
650 07 ‡a551.55 -- Wind and air turbulence.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*80) -- Southern Ocean.‡2udc
651 #7 ‡a(*86) -- Southern Ocean, Australian sector.‡2udc
700 1# ‡aSijp, Willem P.
700 1# ‡aEngland, Matthew H.
773 0# ‡7nnas ‡tJournal of Physical Oceanography. ‡gVol. 43(10) (2013) ‡wSPRI-78712
916 ## ‡a2014/03/17 -- jhr
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220928 ‡bjhr