Cloud Feedbacks, Rapid Adjustments, and the Forcing-Response Relationship in a Transient CO2Reversibility Scenario
暂无分享,去创建一个
[1] John F. B. Mitchell,et al. The time‐dependence of climate sensitivity , 2000 .
[2] Cloud Adjustment and its Role in CO2 Radiative Forcing and Climate Sensitivity: A Review , 2012, Surveys in Geophysics.
[3] G. Martin,et al. A New Boundary Layer Mixing Scheme. Part I: Scheme Description and Single-Column Model Tests , 2000 .
[4] Jonathan M. Gregory,et al. Time Variation of Effective Climate Sensitivity in GCMs , 2008 .
[5] Jason Lowe,et al. Click Here for Full Article , 1989 .
[6] M. Webb,et al. Sensitivity of an Earth system climate model to idealized radiative forcing , 2012 .
[7] T. Delworth,et al. Probing the Fast and Slow Components of Global Warming by Returning Abruptly to Preindustrial Forcing , 2010 .
[8] S. Klein,et al. The Seasonal Cycle of Low Stratiform Clouds , 1993 .
[9] Jason Lowe,et al. The Reversibility of Sea Level Rise , 2013 .
[10] Chao Li,et al. Deep-ocean heat uptake and equilibrium climate response , 2013, Climate Dynamics.
[11] Olivier Boucher,et al. Carbon dioxide induced stomatal closure increases radiative forcing via a rapid reduction in low cloud , 2009 .
[12] S. Bony,et al. On the interpretation of inter-model spread in CMIP5 climate sensitivity estimates , 2013, Climate Dynamics.
[13] A. Keen,et al. Influence of natural variability and the cold start problem on the simulated transient response to increasing CO2 , 1997 .
[14] J. Mitchell. The seasonal response of a general circulation model to changes in CO2 and sea temperatures , 1983 .
[15] Jonathan M. Gregory,et al. Understanding Land–Sea Warming Contrast in Response to Increasing Greenhouse Gases. Part I: Transient Adjustment , 2009 .
[16] S. Bony,et al. Combining ERBE and ISCCP data to assess clouds in the Hadley Centre, ECMWF and LMD atmospheric climate models , 2001 .
[17] Jonathan M. Gregory,et al. A new method for diagnosing radiative forcing and climate sensitivity , 2004 .
[18] K. Taylor,et al. Forcing, feedbacks and climate sensitivity in CMIP5 coupled atmosphere‐ocean climate models , 2012 .
[19] M. Webb,et al. Coupling between subtropical cloud feedback and the local hydrological cycle in a climate model , 2013, Climate Dynamics.
[20] Hajime Okamoto,et al. Fast and slow timescales in the tropical low-cloud response to increasing CO2 in two climate models , 2012, Climate Dynamics.
[21] One- to two-month oscillations in SSMI surface wind speed in western tropical Pacific Ocean , 1994 .
[22] Masahiro Watanabe,et al. Tropospheric adjustment to increasing CO2: its timescale and the role of land–sea contrast , 2013, Climate Dynamics.
[23] G. J. Collatz,et al. Comparison of Radiative and Physiological Effects of Doubled Atmospheric CO2 on Climate , 1996, Science.
[24] Cecilia M. Bitz,et al. The reversibility of sea ice loss in a state‐of‐the‐art climate model , 2011 .
[25] Robert Sausen,et al. On the cold start problem in transient simulations with coupled atmosphere-ocean models , 1992 .
[26] C. Jones,et al. The HadGEM2 family of Met Office Unified Model climate configurations , 2011 .
[27] O. Boucher,et al. Reversibility in an Earth System model in response to CO2 concentration changes , 2012 .
[28] Jonathan M. Gregory,et al. A step‐response simple climate model to reconstruct and interpret AOGCM projections , 2011 .
[29] G. Myhre,et al. New estimates of radiative forcing due to well mixed greenhouse gases , 1998 .
[30] T. Andrews,et al. Evaluating adjusted forcing and model spread for historical and future scenarios in the CMIP5 generation of climate models , 2013 .
[31] Ken Caldeira,et al. Importance of carbon dioxide physiological forcing to future climate change , 2010, Proceedings of the National Academy of Sciences.
[32] J. Gregory. Vertical heat transports in the ocean and their effect on time-dependent climate change , 2000 .
[33] G. Danabasoglu,et al. Equilibrium Climate Sensitivity: Is It Accurate to Use a Slab Ocean Model? , 2009 .
[34] C. Jones,et al. Development and evaluation of an Earth-System model - HadGEM2 , 2011 .
[35] R. Betts,et al. Climate response to the physiological impact of carbon dioxide on plants in the Met Office Unified Model HadCM3 , 2009 .
[36] J. Dufresne,et al. The respective roles of surface temperature driven feedbacks and tropospheric adjustment to CO2 in CMIP5 transient climate simulations , 2013, Climate Dynamics.
[37] M. Schlesinger,et al. Preliminary analysis of experiments on the climatic effects of increased CO2 with an atmospheric general circulation model and a climatological ocean , 1981 .
[38] Piers M. Forster,et al. CO2 forcing induces semi‐direct effects with consequences for climate feedback interpretations , 2008 .
[39] Piers M. Forster,et al. Climate Forcings and Climate Sensitivities Diagnosed from Coupled Climate Model Integrations , 2006 .
[40] W. Ingram,et al. Carbon Dioxide and Climate: Mechanisms of Changes in Cloud , 1992 .
[41] Andrew Gettelman,et al. Evaluation of cloud and water vapor simulations in CMIP5 climate models using NASA “A-Train” satellite observations , 2012 .
[42] Manoj Joshi,et al. An alternative to radiative forcing for estimating the relative importance of climate change mechanisms , 2003 .
[43] M. Watanabe,et al. On the robustness of tropospheric adjustment in CMIP5 models , 2012 .
[44] M. Webb,et al. Origins of differences in climate sensitivity, forcing and feedback in climate models , 2013, Climate Dynamics.
[45] K. Taylor,et al. Contributions of Different Cloud Types to Feedbacks and Rapid Adjustments in CMIP5 , 2012 .
[46] Isaac M. Held,et al. Importance of Ocean Heat Uptake Efficacy to Transient Climate Change , 2010 .
[47] J. Lelieveld,et al. Modelled suppression of boundary-layer clouds by plants in a CO2-rich atmosphere , 2012 .
[48] Adrian Lock,et al. A New Boundary Layer Mixing Scheme. Part II: Tests in Climate and Mesoscale Models , 2000 .
[49] M. Webb,et al. Tropospheric Adjustment Induces a Cloud Component in CO2 Forcing , 2008 .
[50] G. Boer,et al. Climate sensitivity and response , 2003 .
[51] Cecilia M. Bitz,et al. Time-Varying Climate Sensitivity from Regional Feedbacks , 2012 .
[52] M. Webb,et al. The relationship between land-ocean surface temperature contrast and radiative forcing , 2011 .
[53] Ken Caldeira,et al. Why is there a short‐term increase in global precipitation in response to diminished CO2 forcing? , 2011 .
[54] T. Andrews,et al. A regional and global analysis of carbon dioxide physiological forcing and its impact on climate , 2011 .
[55] Peili Wu,et al. Asymmetries in tropical rainfall and circulation patterns in idealised CO2 removal experiments , 2012, Climate Dynamics.
[56] B. McAvaney,et al. On tropospheric adjustment to forcing and climate feedbacks , 2011 .
[57] J. Gregory,et al. Ocean heat uptake and its consequences for the magnitude of sea level rise and climate change , 2012 .
[58] Jonathan M. Gregory,et al. The climate response to CO2 of the Hadley Centre coupled AOGCM with and without flux adjustment , 1997 .
[59] S. Klein,et al. Validation and Sensitivities of Frontal Clouds Simulated by the ECMWF Model , 1999 .
[60] M. Collins,et al. Quantifying global climate feedbacks, responses and forcing under abrupt and gradual CO2 forcing , 2013, Climate Dynamics.
[61] Jason Lowe,et al. Abrupt CO2 experiments as tools for predicting and understanding CMIP5 representative concentration pathway projections , 2013, Climate Dynamics.
[62] C. Bretherton,et al. Fast cloud adjustment to increasing CO2 in a superparameterized climate model , 2012 .
[63] Jonathan M. Gregory,et al. Transient climate response estimated from radiative forcing and observed temperature change , 2008 .
[64] Jonathan M. Gregory,et al. The Role of Climate Sensitivity and Ocean Heat Uptake on AOGCM Transient Temperature Response , 2002 .
[65] J. Hansen,et al. Efficacy of climate forcings , 2005 .