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Record #199617:
- #199617
Main publication details
MARC recordHorizontal density structure and restratification of the Arctic Ocean Surface Layer / Mary-Louise Timmermans, Sylvia Cole, John Toole.
| Title: | Horizontal density structure and restratification of the Arctic Ocean Surface Layer / Mary-Louise Timmermans, Sylvia Cole, John Toole. |
| Author(s): | Timmermans, Mary-Louise. Cole, Sylvia. Toole, John. |
| Date: | 2012. |
| In: | Journal of Physical Oceanography. (2012.), Vol. 42(4) (2012) |
| Abstract: | Reports that ice-tethered profiler (ITP) measurements from Arctic Ocean's Canada Basin indicate ocean surface layer beneath sea ice with significant horizontal density structure. Observed horizontal gradients in density are dynamically important in that they are associated with restratification of surface ocean when dense water flows under light water. Such restratification is prevalent in winter and competes with convective mixing upon buoyancy forcing (e.g. ice growth and brine rejection) and shear-driven mixing when ice moves relative to ocean. |
| Notes: | Journal of Physical Oceanography. Vol. 42(4) :659-668 (2012). |
| Keywords: | 551.326.2 -- Floating ice, formation and decay. 551.46 -- Oceanography, physical. 551.464.5 -- Salinity. 551.465 -- Oceanography, dynamics. 551.465.4 -- Oceanography, stratification. C -- Oceanography, hydrography and hydrology. (*3) -- Arctic regions. (*60) -- Arctic Ocean and adjacent waters. |
| SPRI record no.: | 199617 |
LDR 01795naa#a2200000#a#4500 001 SPRI-199617 005 20240416124149.0 007 ta 008 240416s2012####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-199617 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aTimmermans, Mary-Louise. 245 10 ‡aHorizontal density structure and restratification of the Arctic Ocean Surface Layer /‡cMary-Louise Timmermans, Sylvia Cole, John Toole. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2012. 300 ## ‡ap. 659-668 :‡bill., diags. 500 ## ‡aJournal of Physical Oceanography. Vol. 42(4) :659-668 (2012). 520 3# ‡aReports that ice-tethered profiler (ITP) measurements from Arctic Ocean's Canada Basin indicate ocean surface layer beneath sea ice with significant horizontal density structure. Observed horizontal gradients in density are dynamically important in that they are associated with restratification of surface ocean when dense water flows under light water. Such restratification is prevalent in winter and competes with convective mixing upon buoyancy forcing (e.g. ice growth and brine rejection) and shear-driven mixing when ice moves relative to ocean. 530 ## ‡aAlso issued online ‡uurn:doi:10.1175/JPO-D-11-0125.1‡uhttps://dx.doi.org/10.1175/JPO-D-11-0125.1 650 07 ‡a551.326.2 -- Floating ice, formation and decay.‡2udc 650 07 ‡a551.46 -- Oceanography, physical.‡2udc 650 07 ‡a551.464.5 -- Salinity.‡2udc 650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc 650 07 ‡a551.465.4 -- Oceanography, stratification.‡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 700 1# ‡aCole, Sylvia. 700 1# ‡aToole, John. 773 0# ‡7nnas ‡tJournal of Physical Oceanography. ‡gVol. 42(4) (2012) ‡wSPRI-78712 916 ## ‡a2012/07/02 -- JW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240416 ‡bJW