Link between the double-Intertropical Convergence Zone problem and cloud biases over the Southern Ocean
暂无分享,去创建一个
[1] Martijn Gough. Climate change , 2009, Canadian Medical Association Journal.
[2] Gokhan Danabasoglu,et al. Attribution and Impacts of Upper-Ocean Biases in CCSM3 , 2006 .
[3] A. Arakawa,et al. Peruvian stratus clouds and the tropical Pacific circulation , 1996 .
[4] K. Trenberth,et al. Estimates of Meridional Atmosphere and Ocean Heat Transports , 2001 .
[5] J. Janowiak,et al. The Version 2 Global Precipitation Climatology Project (GPCP) Monthly Precipitation Analysis (1979-Present) , 2003 .
[6] Jialin Lin,et al. The Double-ITCZ Problem in IPCC AR4 Coupled GCMs: Ocean–Atmosphere Feedback Analysis , 2007 .
[7] D. Frierson,et al. Extratropical Influence on ITCZ Shifts in Slab Ocean Simulations of Global Warming , 2012 .
[8] E. Roeckner,et al. Reducing Climatology Bias in an Ocean-Atmosphere CGCM with Improved Coupling Physics. , 2005 .
[9] D. Frierson,et al. Increasing atmospheric poleward energy transport with global warming , 2010 .
[10] Paul R. Houser,et al. Assessing a Satellite-Era Perspective of the Global Water Cycle , 2007 .
[11] M. Latif,et al. The Seasonal Cycle over the Tropical Pacific in Coupled Ocean Atmosphere General Circulation Models , 1995 .
[12] C. Deser,et al. Global warming pattern formation: sea surface temperature and rainfall. , 2010 .
[13] C. Bitz,et al. Influence of high latitude ice cover on the marine Intertropical Convergence Zone , 2005 .
[14] William B. Rossow,et al. Major Characteristics of Southern Ocean Cloud Regimes and Their Effects on the Energy Budget , 2011 .
[15] J. Chiang,et al. Extratropical Cooling, Interhemispheric Thermal Gradients, and Tropical Climate Change , 2012 .
[16] M. Latif,et al. The coupled GCM ECHO-2. Part II: Indian Ocean response to ENSO , 2000 .
[17] J. Thepaut,et al. The ERA‐Interim reanalysis: configuration and performance of the data assimilation system , 2011 .
[18] A. Bodas‐Salcedo,et al. The Surface Downwelling Solar Radiation Surplus over the Southern Ocean in the Met Office Model: The Role of Midlatitude Cyclone Clouds , 2012 .
[19] NCAR CCSM,et al. Increasing Atmospheric Poleward Energy Transport with Global Warming , 2011 .
[20] T. Delworth,et al. Simulated Tropical Response to a Substantial Weakening of the Atlantic Thermohaline Circulation , 2005 .
[21] K. Trenberth,et al. Simulation of Present-Day and Twenty-First-Century Energy Budgets of the Southern Oceans , 2010 .
[22] Guang J. Zhang,et al. Toward mitigating the double ITCZ problem in NCAR CCSM3 , 2006 .
[23] Leon D. Rotstayn,et al. Tropical Rainfall Trends and the Indirect Aerosol Effect , 2002 .
[24] M. Yoshimori,et al. Equilibrium Response of an Atmosphere–Mixed Layer Ocean Model to Different Radiative Forcing Agents: Global and Zonal Mean Response , 2008 .
[25] J. Kay,et al. Coupling between Arctic feedbacks and changes in poleward energy transport , 2011 .
[26] A. Dai. Precipitation Characteristics in Eighteen Coupled Climate Models , 2006 .
[27] Philip J. Rasch,et al. Maintenance of the Intertropical Convergence Zones and the Large-Scale Tropical Circulation on a Water-covered Earth , 1993 .
[28] B. Barkstrom,et al. Clouds and the Earth's Radiant Energy System (CERES): An Earth Observing System Experiment , 1996 .
[29] Mark D. Zelinka,et al. Climate Feedbacks and Their Implications for Poleward Energy Flux Changes in a Warming Climate , 2011 .
[30] Sarah M. Kang,et al. The Response of the ITCZ to Extratropical Thermal Forcing: Idealized Slab-Ocean Experiments with a GCM , 2008 .
[31] J. Janowiak,et al. GPCP Pentad Precipitation analyses: An experimental dataset based on gauge observations and satellite estimates , 2003 .
[32] Huei-Ping Huang,et al. Changes in storm tracks and energy transports in a warmer climate simulated by the GFDL CM2.1 model , 2011 .
[33] R. Stouffer,et al. Response of the ITCZ to Northern Hemisphere cooling , 2006 .
[34] Sarah M. Kang,et al. The Tropical Response to Extratropical Thermal Forcing in an Idealized GCM: The Importance of Radiative Feedbacks and Convective Parameterization , 2009 .
[35] A. Donohoe,et al. What Determines Meridional Heat Transport in Climate Models , 2012 .
[36] A. Rosati,et al. Tropical Sensitivity of a Coupled Model to Specified ISCCP Low Clouds , 2000 .
[37] T. Andrews,et al. An update on Earth's energy balance in light of the latest global observations , 2012 .
[38] M. Latif,et al. The coupled GCM ECHO-2. Part I: The tropical Pacific , 1997 .