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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 |
LDR 01705naa#a2200000#a#4500 001 SPRI-126165 005 20231128094537.0 007 ta 008 231128s1993####gw#a###|#####|0||#0#eng#d 035 ## ‡aSPRI-126165 040 ## ‡aUkCU-P‡beng‡eaacr 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 948 3# ‡a20231128