Atmos. Chem. Phys. Discuss., 9, 24731-24753, 2009
www.atmos-chem-phys-discuss.net/9/24731/2009/
doi:10.5194/acpd-9-24731-2009
© Author(s) 2009. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Estimations of climate sensitivity based on top-of-atmosphere radiation imbalance
B. Lin1, L. Chambers1, P. Stackhouse Jr.1, B. Wielicki1, Y. Hu1, P. Minnis1, N. Loeb1, W. Sun2, G. Potter3, Q. Min4, G. Schuster1, and T.-F. Fan2
1NASA Langley Research Center, Hampton, VA 23681, USA
2SSAI, One Enterprise Parkway, Hampton, VA 23666, USA
3University of California at Davis, Davis, CA 95616, USA
4State University of New York at Albany, Albany, NY 12222, USA

Abstract. Large climate feedback uncertainties limit the accuracy in predicting the response of the Earth's climate to the increase of CO2 concentration within the atmosphere. This study explores a potential to reduce uncertainties in climate sensitivity estimations using energy balance analysis, especially top-of-atmosphere (TOA) radiation imbalance. The time-scales studied generally cover from decade to century, that is, middle-range climate sensitivity is considered, which is directly related to the climate issue caused by atmospheric CO2 change. The significant difference between current analysis and previous energy balance models is that the current study targets at the boundary condition problem instead of solving the initial condition problem. Additionally, climate system memory and deep ocean heat transport are considered. The climate feedbacks are obtained based on the constraints of the TOA radiation imbalance and surface temperature measurements of the present climate.

Currently, there is a lack of high accuracy measurements of TOA radiation imbalance. Available estimations indicate that TOA net radiative heating to the climate system is about 0.85 W/m2. Based on this value, a positive climate feedback with a feedback coefficient ranging from −1.3 to −1.0 W/m2/K is found. The range of feedback coefficient is determined by climate system memory. The longer the memory, the stronger the positive feedback. The estimated time constant of the climate is large (70~120 years) mainly owing to the deep ocean heat transport, implying that the system may be not in an equilibrium state under the external forcing during the industrial era. For the doubled-CO2 climate (or 3.7 W/m2 forcing), the estimated global warming would be 3.1 K if the current estimate of 0.85 W/m2 TOA net radiative heating could be confirmed. With accurate long-term measurements of TOA radiation, the analysis method suggested by this study provides a great potential in the estimations of middle-range climate sensitivity.


Citation: Lin, B., Chambers, L., Stackhouse Jr., P., Wielicki, B., Hu, Y., Minnis, P., Loeb, N., Sun, W., Potter, G., Min, Q., Schuster, G., and Fan, T.-F.: Estimations of climate sensitivity based on top-of-atmosphere radiation imbalance, Atmos. Chem. Phys. Discuss., 9, 24731-24753, doi:10.5194/acpd-9-24731-2009, 2009.
 
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