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Record #139453:
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MARC recordThree-dimensional observations of a deep convective chimney in the Greenland Sea during winter 1988/89 / W.M.L. Morawitz, and five others.
| Title: | Three-dimensional observations of a deep convective chimney in the Greenland Sea during winter 1988/89 / W.M.L. Morawitz, and five others. |
| Author(s): | Morawitz, W. M. L. |
| Date: | 1996. |
| In: | Journal of Physical Oceanography. (1996.), Vol. 26(11) (1996) |
| Abstract: | Temperature data are used to study evolution of 3D temperature field. Chimney structure reaching depths of over 1000 m is seen SW of gyre centre during March, with spatial scale of 50 km and time scale of 10 days. It breaks up in 3-6 days. 1D vertical heat balance adequately describes changes in total heat content from autumn until break-up, when horizontal advection becomes important. 1D mixed layer model reproduces bulk temperature and salinity changes surprisingly well. Comments on salinity changes, energy balance, deep water production rate and presence of Arctic Intermediate Water follow. |
| Notes: | Journal of Physical Oceanography. Vol. 26(11) :2316-2343 (1996). |
| Keywords: | 551.46 -- Oceanography, physical. 551.465 -- Oceanography, dynamics. 551.465.4 -- Oceanography, stratification. C -- Oceanography, hydrography and hydrology. (*3) -- Arctic regions. (*617) -- Greenland Sea and Fram Strait. |
| SPRI record no.: | 139453 |
LDR 01571naa#a2200000#a#4500 001 SPRI-139453 005 20230924211338.0 007 ta 008 230924s1996####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-139453 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aMorawitz, W. M. L. 245 10 ‡aThree-dimensional observations of a deep convective chimney in the Greenland Sea during winter 1988/89 /‡cW.M.L. Morawitz, and five others. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1996. 300 ## ‡ap. 2316-2343 :‡bdiags., tables, map. 500 ## ‡aJournal of Physical Oceanography. Vol. 26(11) :2316-2343 (1996). 520 3# ‡aTemperature data are used to study evolution of 3D temperature field. Chimney structure reaching depths of over 1000 m is seen SW of gyre centre during March, with spatial scale of 50 km and time scale of 10 days. It breaks up in 3-6 days. 1D vertical heat balance adequately describes changes in total heat content from autumn until break-up, when horizontal advection becomes important. 1D mixed layer model reproduces bulk temperature and salinity changes surprisingly well. Comments on salinity changes, energy balance, deep water production rate and presence of Arctic Intermediate Water follow. 650 07 ‡a551.46 -- Oceanography, physical.‡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(*617) -- Greenland Sea and Fram Strait.‡2udc 773 0# ‡7nnas ‡tJournal of Physical Oceanography. ‡gVol. 26(11) (1996) ‡wSPRI-78712 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230924