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Record #126165:

The Late Cenozoic glacial regimes as a combined response to Earth-orbital variations and forced and free CO₂ variations / Barry Saltzman, Mikhail Ya. Verbitsky.

Title: The Late Cenozoic glacial regimes as a combined response to Earth-orbital variations and forced and free CO₂ variations / Barry Saltzman, Mikhail Ya. Verbitsky.
Author(s): Saltzman, Barry.
Verbitsky, Mikhail Ya.
Date: 1993.
Publisher: Berlin: Springer
In: Ice in the climate system. (1993.),
Abstract: Summarizes earlier work aimed at forming self-consistent theory of climatic variations over past 5 Ma; this involves two basic levels of variability: quasi-equilibrium changes in CO₂ forced by slow tectonic processes, and non-equilibrium variations of fuller climatic system involving ice, bedrock, ocean, and CO₂ as interactive, closed, nonlinear system. To these studies has been added more expanded discussion of part of theory dealing with slow tectonic evolution of CO₂. In addition, structural stability properties of model are described, showing bifurcations that can lead to major regime changes that occurred during Late Cenozoic.
Notes:

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

Keywords: 551.336 -- Ice ages.
551.77 -- Cenozoic.
551.583 -- Climatic changes.
551.588.5 -- Climate, relationship with ice.
519.673 -- Modelling.
E7 -- Glaciology: glacial geology and ice ages.
SPRI record no.: 126165

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100 1# ‡aSaltzman, Barry.
245 14 ‡aThe Late Cenozoic glacial regimes as a combined response to Earth-orbital variations and forced and free CO₂ variations /‡cBarry Saltzman, Mikhail Ya. Verbitsky.
260 ## ‡aBerlin :‡bSpringer,‡c1993.
300 ## ‡ap. 343-361 :‡bdiags., table.
490 0# ‡aNATO ASI Series. Series I, Global environmental change ;‡v12
500 ## ‡aIn: Ice in the climate system / W. Richard Peltier, ed.
520 3# ‡aSummarizes earlier work aimed at forming self-consistent theory of climatic variations over past 5 Ma; this involves two basic levels of variability: quasi-equilibrium changes in CO₂ forced by slow tectonic processes, and non-equilibrium variations of fuller climatic system involving ice, bedrock, ocean, and CO₂ as interactive, closed, nonlinear system. To these studies has been added more expanded discussion of part of theory dealing with slow tectonic evolution of CO₂. In addition, structural stability properties of model are described, showing bifurcations that can lead to major regime changes that occurred during Late Cenozoic.
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.77 -- Cenozoic.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
700 1# ‡aVerbitsky, Mikhail Ya.
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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