Abstract
Projections of future climate change by climate system models depend on the sensitivities of models to specified greenhouse gases. To reveal and understand the different climate sensitivities of version 2 of the grid-point and spectral Flexible Global Ocean–Atmosphere–Land System Model, FGOALS-g2 and FGOALS-s2, respectively, which were developed by the National Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics/Institute of Atmospheric Physics (LASG/IAP), global mean surface air temperature responses to idealized CO2 forcing are investigated by using the output of abruptly quadrupling CO2 experiments. The globally averaged near-surface air temperature is characterized by a fast response to CO2 forcing during the first 20 years and a slow response afterward. The climate sensitivity, defined as the equilibrium temperature under doubled CO2 forcing, estimated by Gregory regression method, is approximately 3.7 K in FGOALS-g2 and 4.5 K in FGOALS-s2. The larger sensitivity of FGOALS-s2 is mainly attributed to a weaker negative long wave clear-sky feedback and stronger positive shortwave clear-sky feedback at the fast-response stage, as evidenced by the more rapid response of water vapor increase and sea-ice decrease in FGOALS-s2 than that in FGOALS-g2. At the slow-response stage in FGOALS-s2, larger responses of increasing total cloud fraction and condensed water path result in a stronger negative shortwave cloud feedback, which tends to reduce the sensitivity of the model.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Similar content being viewed by others
Acknowledgments
This study was supported by the Strategic Priority Research Program—Climate Change: Carbon Budget and Related Issues of the Chinese Academy of Sciences under Grant No. XDA05110301.
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2014 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Chen, X., Guo, Z., Zhou, T. (2014). Climate Sensitivity of the Flexible Global Ocean–Atmosphere–Land System Model. In: Zhou, T., Yu, Y., Liu, Y., Wang, B. (eds) Flexible Global Ocean-Atmosphere-Land System Model. Springer Earth System Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-41801-3_26
Download citation
DOI: https://doi.org/10.1007/978-3-642-41801-3_26
Published:
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-41800-6
Online ISBN: 978-3-642-41801-3
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)