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Record #126160:

Hydrological cycle scenarios, deep ocean circulation, and century/millennium climate change: a simulation study using an ocean--atmosphere--ice sheet model / Huaxiao Wang, G. Edward Birchfield, Jonathan J. Rich.

Title: Hydrological cycle scenarios, deep ocean circulation, and century/millennium climate change: a simulation study using an ocean--atmosphere--ice sheet model / Huaxiao Wang, G. Edward Birchfield, Jonathan J. Rich.
Author(s): Wang, Huaxiao.
Birchfield, G. Edward.
Rich, Jonathan J.
Date: 1993.
Publisher: Berlin: Springer
In: Ice in the climate system. (1993.),
Abstract: Rapid climate changes during most of last glaciation and during last deglaciation, seen in Greenland ice cores and deep-sea sediment core in North Atlantic, are probably caused by dynamical instability of climate system itself. Here, oscillatory feedback mechanisms are described, using simple coupled ocean--atmosphere--ice-sheet energy--salt-balance model, which explains these climate changes.
Notes:

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

Keywords: 551.58 -- Climatology.
551.583 -- Climatic changes.
551.583.3 -- Climatic changes, Quaternary.
551.588.5 -- Climate, relationship with ice.
551.465.7 -- Oceanography, energy budget.
519.673 -- Modelling.
E9 -- Glaciology: meteorology and climatology.
SPRI record no.: 126160

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100 1# ‡aWang, Huaxiao.
245 10 ‡aHydrological cycle scenarios, deep ocean circulation, and century/millennium climate change :‡ba simulation study using an ocean--atmosphere--ice sheet model /‡cHuaxiao Wang, G. Edward Birchfield, Jonathan J. Rich.
260 ## ‡aBerlin :‡bSpringer,‡c1993.
300 ## ‡ap. 237-254 :‡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# ‡aRapid climate changes during most of last glaciation and during last deglaciation, seen in Greenland ice cores and deep-sea sediment core in North Atlantic, are probably caused by dynamical instability of climate system itself. Here, oscillatory feedback mechanisms are described, using simple coupled ocean--atmosphere--ice-sheet energy--salt-balance model, which explains these climate changes.
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with 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
700 1# ‡aBirchfield, G. Edward.
700 1# ‡aRich, Jonathan J.
773 0# ‡7nnam ‡aW. Richard Peltier, ed. ‡tIce in the climate system. ‡dBerlin : Springer, 1993. ‡wSPRI-126141
917 ## ‡aUnenhanced record from Muscat, imported 2019
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