Back to Search Start Over

Probability distributions for carbon emissions and atmospheric response.

Authors :
Singer, Clifford E.
Rethinaraj, T. S. Gopi
Addy, Samuel
Durham, David
Isik, Murat
Khanna, Madhu
Kuehl, Brandon
Jianding Luo
Wilma Quimio
Rajendran, Kothavari
Ramirez, Donna
Ji Qiang
Scheffran, Jürgen
Tiouririne, T. Nedjla
Junli Zhang
Source :
Climatic Change. Jun2008, Vol. 88 Issue 3/4, p309-342. 34p. 7 Charts, 11 Graphs.
Publication Year :
2008

Abstract

Probability distributions for carbon burning, atmospheric CO2, and global average temperature are produced by time series calibration of models of utility optimization and carbon and heat balance using log-linear production functions. Population growth is used to calibrate a logistically evolving index of development that influences production efficiency. Energy production efficiency also includes a coefficient that decreases linearly with decreasing carbon intensity of energy production. This carbon intensity is a piecewise linear function of fossil carbon depletion. That function is calibrated against historical data and extrapolated by sampling a set of hypotheses about the impact on the carbon intensity of energy production of depleting fluid fossil fuel resources and increasing cumulative carbon emissions. Atmospheric carbon balance is determined by a first order differential equation with carbon use rates and cumulative carbon use as drivers. Atmospheric CO2 is a driver in a similar heat balance. Periodic corrections are included where required to make residuals between data and model results indistinguishable from independently and identically distributed normal distributions according to statistical tests on finite Fourier power spectrum amplitudes and nearest neighbor correlations. Asymptotic approach to a sustainable non-fossil energy production is followed for a global disaggregation into a tropical/developing and temperate/more-developed Electronic supplementary material The online version of this article region. The increase in the uncertainty of global average temperature increases nearly quadratically with the increase in the temperature from the present through the next two centuries. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
01650009
Volume :
88
Issue :
3/4
Database :
Academic Search Index
Journal :
Climatic Change
Publication Type :
Academic Journal
Accession number :
32920017
Full Text :
https://doi.org/10.1007/s10584-008-9410-4