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Record #126170:

The glacial ocean: a study with a zonally averaged, three-basin ocean circulation model / T. Fichefet, S. Hovine.

Title: The glacial ocean: a study with a zonally averaged, three-basin ocean circulation model / T. Fichefet, S. Hovine.
Author(s): Fichefet, T.
Hovine, S.
Date: 1993.
Publisher: Berlin: Springer
In: Ice in the climate system. (1993.),
Abstract: Atlantic, Indian and Pacific basins are separately resolved and are connected in southern hemisphere by circumpolar channel through which mass, heat and salt are exchanged. Under present-day boundary condition, model reproduces global conveyer belt, and simulated temperature and salinity fields and computed meridional heat transport are in general agreement with observations. When glacial conditions for temperature and salinity are used to force model, significant changes occur in circulation patterns. All changes compare favourably with existing geological reconstructions.
Notes:

In: Ice in the climate system / W. Richard Peltier, ed.

Keywords: 551.46 -- Oceanography, physical.
551.465.45 -- Water masses.
551.583 -- Climatic changes.
551.588.5 -- Climate, relationship with ice.
551.461.8 -- Palaeo-oceanography.
519.673 -- Modelling.
C -- Oceanography, hydrography and hydrology.
(*80) -- Southern Ocean.
SPRI record no.: 126170

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100 1# ‡aFichefet, T.
245 14 ‡aThe glacial ocean :‡ba study with a zonally averaged, three-basin ocean circulation model /‡cT. Fichefet, S. Hovine.
260 ## ‡aBerlin :‡bSpringer,‡c1993.
300 ## ‡ap. 433-458 :‡bdiags.
490 0# ‡aNATO ASI Series. Series I, Global environmental change ;‡v12
500 ## ‡aIn: Ice in the climate system / W. Richard Peltier, ed.
520 3# ‡aAtlantic, Indian and Pacific basins are separately resolved and are connected in southern hemisphere by circumpolar channel through which mass, heat and salt are exchanged. Under present-day boundary condition, model reproduces global conveyer belt, and simulated temperature and salinity fields and computed meridional heat transport are in general agreement with observations. When glacial conditions for temperature and salinity are used to force model, significant changes occur in circulation patterns. All changes compare favourably with existing geological reconstructions.
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465.45 -- Water masses.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a551.461.8 -- Palaeo-oceanography.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*80) -- Southern Ocean.‡2udc
700 1# ‡aHovine, S.
773 0# ‡7nnam ‡aW. Richard Peltier, ed. ‡tIce in the climate system. ‡dBerlin : Springer, 1993. ‡wSPRI-126141
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220929