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Record #205611:
Time-mean flow as the prevailing contribution to the poleward heat flux across the southern flank of the Antarctic Circumpolar Current: a case study in the Fawn Trough, Kerguelen Plateau / H. Sekma, and 3 others.
Title: | Time-mean flow as the prevailing contribution to the poleward heat flux across the southern flank of the Antarctic Circumpolar Current: a case study in the Fawn Trough, Kerguelen Plateau / H. Sekma, and 3 others. |
Author(s): | Sekma, H. |
Date: | 2013. |
In: | Journal of Physical Oceanography. (2013.), Vol. 43(3) (2013) |
Abstract: | Describes study analysing moored current meter data obtained in Fawn Trough, Kerguelen Plateau, to estimate cross-stream heat flux caused by time-mean flow and transient eddies. Results show that poleward eddy heat flux is negligible, while that from mean flow is overwhelming. Discusses reason for this, and circumpolar implications of observations. |
Notes: | Journal of Physical Oceanography. Vol. 43(3) :583-601 (2013). |
Keywords: | 551.46 -- Oceanography, physical. 551.46.06 -- Oceanography, observational data. 551.465 -- Oceanography, dynamics. 551.465.15 -- Turbulence and eddies. 551.465.4 -- Oceanography, stratification. 551.465.7 -- Oceanography, energy budget. 551.465.5 -- Ocean currents. C -- Oceanography, hydrography and hydrology. (*7) -- Antarctic regions. (*80) -- Southern Ocean. (*84) -- South Indian Ocean. |
SPRI record no.: | 205611 |
LDR 01767naa#a2200000#a#4500 001 SPRI-205611 005 20240329022335.0 007 ta 008 240329s2013####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-205611 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aSekma, H. 245 10 ‡aTime-mean flow as the prevailing contribution to the poleward heat flux across the southern flank of the Antarctic Circumpolar Current :‡ba case study in the Fawn Trough, Kerguelen Plateau /‡cH. Sekma, and 3 others. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2013. 300 ## ‡ap. 583-601 :‡bill., diags., tables, maps. 500 ## ‡aJournal of Physical Oceanography. Vol. 43(3) :583-601 (2013). 520 3# ‡aDescribes study analysing moored current meter data obtained in Fawn Trough, Kerguelen Plateau, to estimate cross-stream heat flux caused by time-mean flow and transient eddies. Results show that poleward eddy heat flux is negligible, while that from mean flow is overwhelming. Discusses reason for this, and circumpolar implications of observations. 530 ## ‡aAlso issued online ‡uurn:doi:10.1175/JPO-D-12-0125.1‡uhttps://dx.doi.org/10.1175/JPO-D-12-0125.1 650 07 ‡a551.46 -- Oceanography, physical.‡2udc 650 07 ‡a551.46.06 -- Oceanography, observational data.‡2udc 650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc 650 07 ‡a551.465.15 -- Turbulence and eddies.‡2udc 650 07 ‡a551.465.4 -- Oceanography, stratification.‡2udc 650 07 ‡a551.465.7 -- Oceanography, energy budget.‡2udc 650 07 ‡a551.465.5 -- Ocean currents.‡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(*84) -- South Indian Ocean.‡2udc 773 0# ‡7nnas ‡tJournal of Physical Oceanography. ‡gVol. 43(3) (2013) ‡wSPRI-78712 916 ## ‡a2013/12/11 -- JR 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240329 ‡bJR