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The climatic effect of co2: A different viewstar, open
Hugh W. Ellsaesser†, a
a4293 Stanford Way, Livermore, CA 94550 U.S.A.
Received 27 June 1983;
revised 4 August 1983.
Available online 14 April 2003.
Abstract
The current eager acceptance of oceanic thermal lag as the “explanation” as to why CO2 warming remains undetected, reemphasizes that the atmosphere cannot warm until the oceans do. The logical implication follows that most current climate models are lacking in relevance; they have not been constructed with ocean surface temperature as the fundamental variable. When the problem is attacked from this view, sensitivity to CO2 is significantly reduced; a position also strongly supported by the available palaeoclimatic data.
star, openThis paper was prepared originally for presentation at the Second Conference on Climate Variations, 10–14 January 1983, New Orleans, LA.
† Dr. Ellsaesser is employed by the Lawrence Livermore National Laboratory, P.O. Box 808, Livermore, CA 94550, U.S.A.
ScienceDirect - Atmospheric Environment (1967) : The climatic effect of co2: A different view
Copyright © 2011 Elsevier B.V. All rights reserved. SciVerse® is a registered trademark of Elsevier Properties S.A., used under license. ScienceDirect® is a registered trademark of Elsevier B.V.
SpringerLink - Theoretical and Applied Climatology, Volume 38, Number 1
SpringerLink - Climatic Change, Volume 21, Number 4
SpringerLink - Environmental Geology, Volume 58, Number 6
Paper: Recent Energy Balance of Earth
Inter Research*»*CR*»*v23*»*n1*»*p1-9
SpringerLink - Central European Journal of Physics, Volume 3, Number 2
Multi-Science Publishing - Journal Article
Multi-Science Publishing - Journal Article
AMS Journals Online - The Aerial Fertilization Effect of CO<sub>2</sub> and Its Implications for Global Carbon Cycling and Maximum Greenhouse Warming
An updated Antarctic melt record through 2009 and its linkages to high-latitude and tropical climate variability
First survey of Antarctic sub-ice shelf sediments reveals mid-Holocene ice shelf retreat -- Pudsey and Evans 29 (9): 787 -- Geology
Historical variability of sea ice edge position in the Nordic Seas
http://www.jstor.org/pss/1550979
http://www.ingentaconnect.com/content/nrc/cjes/2008/00000045/00000011/art00015
Hugh W. Ellsaesser†, a
a4293 Stanford Way, Livermore, CA 94550 U.S.A.
Received 27 June 1983;
revised 4 August 1983.
Available online 14 April 2003.
Abstract
The current eager acceptance of oceanic thermal lag as the “explanation” as to why CO2 warming remains undetected, reemphasizes that the atmosphere cannot warm until the oceans do. The logical implication follows that most current climate models are lacking in relevance; they have not been constructed with ocean surface temperature as the fundamental variable. When the problem is attacked from this view, sensitivity to CO2 is significantly reduced; a position also strongly supported by the available palaeoclimatic data.
star, openThis paper was prepared originally for presentation at the Second Conference on Climate Variations, 10–14 January 1983, New Orleans, LA.
† Dr. Ellsaesser is employed by the Lawrence Livermore National Laboratory, P.O. Box 808, Livermore, CA 94550, U.S.A.
ScienceDirect - Atmospheric Environment (1967) : The climatic effect of co2: A different view
Copyright © 2011 Elsevier B.V. All rights reserved. SciVerse® is a registered trademark of Elsevier Properties S.A., used under license. ScienceDirect® is a registered trademark of Elsevier B.V.
SpringerLink - Theoretical and Applied Climatology, Volume 38, Number 1
SpringerLink - Climatic Change, Volume 21, Number 4
SpringerLink - Environmental Geology, Volume 58, Number 6
Paper: Recent Energy Balance of Earth
Inter Research*»*CR*»*v23*»*n1*»*p1-9
SpringerLink - Central European Journal of Physics, Volume 3, Number 2
Multi-Science Publishing - Journal Article
Multi-Science Publishing - Journal Article
AMS Journals Online - The Aerial Fertilization Effect of CO<sub>2</sub> and Its Implications for Global Carbon Cycling and Maximum Greenhouse Warming
An updated Antarctic melt record through 2009 and its linkages to high-latitude and tropical climate variability
First survey of Antarctic sub-ice shelf sediments reveals mid-Holocene ice shelf retreat -- Pudsey and Evans 29 (9): 787 -- Geology
Historical variability of sea ice edge position in the Nordic Seas
http://www.jstor.org/pss/1550979
http://www.ingentaconnect.com/content/nrc/cjes/2008/00000045/00000011/art00015
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