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Record #152054:

On the parameterisation of oceanic sensible heat loss to the atmosphere and to ice in an ice-covered mixed layer in winter / Bert Rudels, Hans J. Friedrich, Dagmar Hainbucher, Gerrit Lohmann.

Title: On the parameterisation of oceanic sensible heat loss to the atmosphere and to ice in an ice-covered mixed layer in winter / Bert Rudels, Hans J. Friedrich, Dagmar Hainbucher, Gerrit Lohmann.
Author(s): Rudels, Bert.
Friedrich, Hans J.
Hainbucher, Dagmar.
Lohmann, Gerrit.
Date: 1999.
In: European subpolar ocean programme : Sea ice-ocean interactions, deep convection and carbon cycling in the Greenland Sea. (1999.), Vol. 46(6-7) (1999)
Abstract: Discusses interactions between ice cover and entrainment during winter, with heat loss to atmosphere. Buoyancy input at sea surface due to ice melt is at minimum, model finds this corresponds to constant fraction of heat loss going to ice melt, leading to deep convection event. Compares conditions in Weddell Sea and Greenland Sea.
Notes:

European subpolar ocean programme : Sea ice-ocean interactions, deep convection and carbon cycling in the Greenland Sea. Vol. 46(6-7) :1385-1425 (1999).

Keywords: 551.32 -- Glaciology.
551.326.7 -- Sea ice.
551.465.7 -- Oceanography, energy budget.
519.673 -- Modelling.
E9 -- Glaciology: meteorology and climatology.
(*826) -- Weddell Sea.
(*617) -- Greenland Sea and Fram Strait.
Location(s): SCO: SPRI-SHF: (*617)
SPRI record no.: 152054

MARCXML

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001 SPRI-152054
005 20220928162831.0
007 ta
008 220928s1999####xx#a##|##|###|0||#0|eng#d
035 ## ‡aSPRI-152054
040 ## ‡aUkCU-P‡beng‡eaacr
245 00 ‡aOn the parameterisation of oceanic sensible heat loss to the atmosphere and to ice in an ice-covered mixed layer in winter /‡cBert Rudels, Hans J. Friedrich, Dagmar Hainbucher, Gerrit Lohmann.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1999.
300 ## ‡ap. 1385-1425 :‡bdiags., tables.
500 ## ‡aEuropean subpolar ocean programme : Sea ice-ocean interactions, deep convection and carbon cycling in the Greenland Sea. Vol. 46(6-7) :1385-1425 (1999).
520 3# ‡aDiscusses interactions between ice cover and entrainment during winter, with heat loss to atmosphere. Buoyancy input at sea surface due to ice melt is at minimum, model finds this corresponds to constant fraction of heat loss going to ice melt, leading to deep convection event. Compares conditions in Weddell Sea and Greenland Sea.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.465.7 -- Oceanography, energy budget.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local
651 #7 ‡a(*826) -- Weddell Sea.‡2udc
651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc
700 1# ‡aRudels, Bert.
700 1# ‡aFriedrich, Hans J.
700 1# ‡aHainbucher, Dagmar.
700 1# ‡aLohmann, Gerrit.
773 0# ‡7nnam ‡tEuropean subpolar ocean programme : Sea ice-ocean interactions, deep convection and carbon cycling in the Greenland Sea. ‡gVol. 46(6-7) (1999) ‡wSPRI-150747
852 7# ‡2camdept‡bSCO‡cSPRI-SHF‡h(*617)‡9Create 1 item record‡0Migrate
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220928