The CSIRO Mk3L climate system model version 1.0 - Part 2: Response to external forcings
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S. Phipps | L. Rotstayn | A. Hirst | H. B. Gordon | J. Roberts | W. Budd | H. Gordon
[1] Steven J. Phipps,et al. Climate drift in the CMIP3 models , 2012 .
[2] J. Jungclaus,et al. Evolution of the seasonal temperature cycle in a transient Holocene simulation: orbital forcing and sea-ice , 2011 .
[3] Susanne L. Weber,et al. The stability of the MOC as diagnosed from model projections for pre-industrial, present and future climates , 2011 .
[4] R. S. Thompson,et al. Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis , 2011 .
[5] Ed Hawkins,et al. Correction to “Bistability of the Atlantic overturning circulation in a global climate model and links to ocean freshwater transport” , 2011 .
[6] Leon D. Rotstayn,et al. The CSIRO Mk3L climate system model version 1.0 – Part 1: Description and evaluation , 2011 .
[7] M. Schulz,et al. Holocene evolution of the Southern Hemisphere westerly winds in transient simulations with global climate models , 2011 .
[8] Ed Hawkins,et al. Bistability of the Atlantic overturning circulation in a global climate model and links to ocean freshwater transport , 2011 .
[9] V. Brovkin,et al. The effect of a dynamic background albedo scheme on Sahel/Sahara precipitation during the mid-Holocene , 2010 .
[10] Heinrich Widmann,et al. Climate and carbon-cycle variability over the last millennium , 2010 .
[11] P. Yiou,et al. Influence of solar variability, CO 2 and orbital forcing between 1000 and 1850 AD in the IPSLCM4 model , 2010 .
[12] T. Stocker,et al. Variations of the Atlantic meridional overturning circulation in control and transient simulations of the last millennium , 2010 .
[13] W. Landman. Climate change 2007: the physical science basis , 2010 .
[14] John M. Wallace,et al. Identifying Signatures of Natural Climate Variability in Time Series of Global-Mean Surface Temperature: Methodology and Insights , 2009 .
[15] C. Timmreck,et al. Limited temperature response to the very large AD 1258 volcanic eruption , 2009 .
[16] C. Fröhlich,et al. Total solar irradiance during the Holocene , 2009 .
[17] A. Wittenberg. Are historical records sufficient to constrain ENSO simulations? , 2009 .
[18] W. Soon,et al. Centennial Variations of the Global Monsoon Precipitation in the Last Millennium: Results from ECHO-G Model , 2009 .
[19] G. Danabasoglu,et al. Equilibrium Climate Sensitivity: Is It Accurate to Use a Slab Ocean Model? , 2009 .
[20] C. Ammann,et al. Understanding Changes in the Asian Summer Monsoon over the Past Millennium: Insights from a Long-Term Coupled Model Simulation* , 2009 .
[21] Jonathan M. Gregory,et al. Transient climate response estimated from radiative forcing and observed temperature change , 2008 .
[22] V. Brovkin,et al. Comment on "Climate-Driven Ecosystem Succession in the Sahara: The Past 6000 Years" , 2008, Science.
[23] Helen McGregor,et al. Mid‐Holocene ENSO: Issues in quantitative model‐proxy data comparisons , 2008 .
[24] E. Guilyardi,et al. ENSO at 6ka and 21ka from ocean–atmosphere coupled model simulations , 2008 .
[25] B. Rumes,et al. Climate-Driven Ecosystem Succession in the Sahara: The Past 6000 Years , 2008, Science.
[26] X. Liang,et al. Rectification of the Bias in the Wavelet Power Spectrum , 2007 .
[27] R. Betts,et al. Changes in Atmospheric Constituents and in Radiative Forcing. Chapter 2 , 2007 .
[28] John F. B. Mitchell,et al. THE WCRP CMIP3 Multimodel Dataset: A New Era in Climate Change Research , 2007 .
[29] T. Fichefet,et al. Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum – Part 2: feedbacks with emphasis on the location of the ITCZ and mid- and high latitudes heat budget , 2007 .
[30] Yan Zhao,et al. Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum - Part 1: experiments and large-scale features , 2007 .
[31] S. Solanki,et al. Grand minima and maxima of solar activity: new observational constraints , 2007, 0706.0385.
[32] A. Kitoh,et al. El Niño–Southern Oscillation Simulation at 6000 Years before Present with the MRI-CGCM2.3: Effect of Flux Adjustment , 2007 .
[33] Yan Feng,et al. Have Australian rainfall and cloudiness increased due to the remote effects of Asian anthropogenic aerosols , 2007 .
[34] A. Robock,et al. Volcanic forcing of climate over the past 1500 years: An improved ice core-based index for climate models , 2006 .
[35] E. Maier‐Reimer,et al. Dynamics of the terrestrial biosphere, climate and atmospheric CO2 concentration during interglacials: a comparison between Eemian and Holocene , 2006 .
[36] Yi Wang,et al. On the cause of abrupt vegetation collapse in North Africa during the Holocene: Climate variability vs. vegetation feedback , 2006 .
[37] D. Frank,et al. Summer temperature variations in the European Alps, A.D. 755-2004 , 2006 .
[38] Paul Steele,et al. Law Dome CO2, CH4 and N2O ice core records extended to 2000 years BP , 2006 .
[39] S. Levis,et al. Last Glacial Maximum and Holocene Climate in CCSM3 , 2006 .
[40] Frank O. Bryan,et al. Response of the North Atlantic Thermohaline Circulation and Ventilation to Increasing Carbon Dioxide in CCSM3 , 2006 .
[41] R. Schneider,et al. Orbitally driven insolation forcing on Holocene climate trends: Evidence from alkenone data and climate modeling , 2006 .
[42] J. Fyfe,et al. Simulated changes in the extratropical Southern Hemisphere winds and currents , 2006 .
[43] M. Latif,et al. Tropical Pacific Decadal Variability and the Subtropical–Tropical Cells , 2005 .
[44] Charles S. Zender,et al. Impact of Desert Dust Radiative Forcing on Sahel Precipitation , 2005 .
[45] Andrei P. Sokolov,et al. A model intercomparison of changes in the Atlantic thermohaline circulation in response to increasing atmospheric CO2 concentration , 2005 .
[46] J. Lean,et al. Modeling the Sun’s Magnetic Field and Irradiance since 1713 , 2005 .
[47] B. Santer,et al. Effect of climate sensitivity on the Response to Volcanic Forcing , 2005 .
[48] A. Robock. Cooling following large volcanic eruptions corrected for the effect of diffuse radiation on tree rings , 2005 .
[49] G. Bonan,et al. Soil feedback drives the mid-Holocene North African monsoon northward in fully coupled CCSM2 simulations with a dynamic vegetation model , 2004 .
[50] G. Meehl,et al. Response of the Atlantic Thermohaline Circulation to Increased Atmospheric CO2 in a Coupled Model , 2004 .
[51] Gerrit Lohmann,et al. Acceleration technique for Milankovitch type forcing in a coupled atmosphere-ocean circulation model: method and application for the Holocene , 2004 .
[52] G. Flato,et al. Sea-ice and its response to CO2 forcing as simulated by global climate models , 2004 .
[53] N. Noblet-Ducoudré,et al. Some mechanisms of mid-Holocene climate change in Europe, inferred from comparing PMIP models to data , 2004 .
[54] J. Palutikof,et al. Model intercomparison for the present day, the mid-Holocene, and the Last Glacial Maximum over western Europe , 2004 .
[55] Jonathan M. Gregory,et al. A new method for diagnosing radiative forcing and climate sensitivity , 2004 .
[56] G. Schmidt,et al. Volcanic and Solar Forcing of Climate Change during the Preindustrial Era , 2003 .
[57] R. Wood,et al. Global warming and thermohaline circulation stability , 2003, Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.
[58] Xingren Wu,et al. Response of the antarctic circumpolar current transport to global warming in a coupled model , 2002 .
[59] David M. Anderson,et al. Variability of El Niño/Southern Oscillation activity at millennial timescales during the Holocene epoch , 2002, Nature.
[60] M. Kanamitsu,et al. NCEP–DOE AMIP-II Reanalysis (R-2) , 2002 .
[61] T. V. Ommen,et al. Observed climate variability and change , 2002 .
[62] Xingren Wu,et al. Collapse and reorganisation of the Southern Ocean overturning under global warming in a coupled model , 2001 .
[63] Leon D. Rotstayn,et al. Indirect Aerosol Forcing, Quasi Forcing, and Climate Response , 2001 .
[64] E. Cook,et al. Variability in the El Niño-Southern Oscillation Through a Glacial-Interglacial Cycle , 2001, Science.
[65] G. Ramstein,et al. Mid-Holocene and Last Glacial Maximum African monsoon changes as simulated within the Paleoclimate Modelling Intercomparison Project , 2000 .
[66] K. Shine. Radiative Forcing of Climate Change , 2000 .
[67] John F. B. Mitchell,et al. The time‐dependence of climate sensitivity , 2000 .
[68] Judith Lean,et al. Evolution of the Sun's Spectral Irradiance Since the Maunder Minimum , 2000 .
[69] John E. Kutzbach,et al. Modeling climate shift of El Nino variability in the Holocene , 2000 .
[70] Crowley,et al. Atmospheric science: Methane rises from wetlands , 2011, Nature.
[71] A. Robock. Volcanic eruptions and climate , 2000 .
[72] D. Jolly,et al. Mid‐Holocene and glacial‐maximum vegetation geography of the northern continents and Africa , 2000 .
[73] G. Meehl,et al. The Coupled Model Intercomparison Project (CMIP) , 2000 .
[74] N. Noblet,et al. Synergistic feedbacks from ocean and vegetation on the African Monsoon response to Mid‐Holocene insolation , 1999 .
[75] S. Manabe,et al. Response of a Coupled Ocean–Atmosphere Model to Increasing Atmospheric Carbon Dioxide: Sensitivity to the Rate of Increase , 1999 .
[76] Sandy P. Harrison,et al. Monsoon changes for 6000 years ago: Results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP) , 1999 .
[77] P. Braconnot,et al. Mid-Holocene climate in Europe: what can we infer from PMIP model-data comparisons? , 1999 .
[78] I. Watterson,et al. A comparison of present and doubled CO2 climates and feedbacks simulated by three general circulation models , 1999 .
[79] Mark B. Abbott,et al. An ;15,000-Year Record of El Nino—Driven Alluviation in Southwestern Ecuador , 1999 .
[80] I. C. Prentice,et al. BIOME 6000: reconstructing global mid‐Holocene vegetation patterns from palaeoecological records , 1998 .
[81] J. Kutzbach,et al. Intercomparison of Simulated Global Vegetation Distributions in Response to 6 kyr BP Orbital Forcing , 1998 .
[82] I. Prentice,et al. Biome reconstruction from pollen and plant macrofossil data for Africa and the Arabian peninsula at 0 and 6000 years , 1998 .
[83] S. Harrison,et al. Simulated climate and biomes of Africa during the late quaternary: comparison with pollen and lake status data , 1998 .
[84] Sandy P. Harrison,et al. Mid‐Holocene land‐surface conditions in northern Africa and the Arabian Peninsula: A data set for the analysis of biogeophysical feedbacks in the climate system , 1998 .
[85] Jonathan M. Gregory,et al. The climate response to CO2 of the Hadley Centre coupled AOGCM with and without flux adjustment , 1997 .
[86] J. Wallace,et al. ENSO-like Interdecadal Variability: 1900–93 , 1997 .
[87] S. O’Farrell,et al. Transient Climate Change in the CSIRO Coupled Model with Dynamic Sea Ice , 1997 .
[88] S. Harrison,et al. An evaluation of the simulated water balance of Eurasia and northern Africa at 6000 y BP using lake status data , 1996 .
[89] Ge Yu,et al. The climate of Europe 6000 years ago , 1996 .
[90] J. Lean,et al. Reconstruction of solar irradiance since 1610: Implications for climate change , 1995 .
[91] J. Shulmeister,et al. Pollen evidence from tropical Australia for the onset of an ENSO-dominated climate at c. 4000 BP , 1995 .
[92] Syukuro Manabe,et al. Century-scale effects of increased atmospheric C02 on the ocean–atmosphere system , 1993, Nature.
[93] P. Minnis,et al. Radiative Climate Forcing by the Mount Pinatubo Eruption , 1993, Science.
[94] Robert Sausen,et al. On the cold start problem in transient simulations with coupled atmosphere-ocean models , 1992 .
[95] R. Stothers. The Great Tambora Eruption in 1815 and Its Aftermath , 1984, Science.
[96] K. Bryan. Accelerating the Convergence to Equilibrium of Ocean-Climate Models , 1984 .
[97] André Berger,et al. Long-term variations of daily insolation and Quaternary climatic changes , 1978 .
[98] John A. Eddy,et al. The Maunder Minimum , 1976, Science.
[99] Model Development Discussions , 2013 .
[100] G. Faluvegi,et al. Global signatures and dynamical origins of the Little Ice Age and Medieval Climate Anomaly. , 2009, Science.
[101] W. Collins,et al. Global climate projections , 2007 .
[102] I. Smith. Global climate modelling within CSIRO: 1981 to 2006 , 2007 .
[103] K. Trenberth,et al. Observations: Surface and Atmospheric Climate Change , 2007 .
[104] J. Guiot,et al. under a Creative Commons License. Climate of the Past Mid-Holocene climate change in Europe: a data-model comparison , 2007 .
[105] I. Watterson,et al. Effective sensitivity and heat capacity in the response of climate models to greenhouse gas and aerosol forcings , 2005 .
[106] Syukuro Manabe,et al. Equilibrium response of thermohaline circulation to large changes in atmospheric CO2 concentration , 2004 .
[107] Daohua Bi. Transient and long-term behaviour of the world ocean under global warming , 2002 .
[108] John S. Woollen,et al. NCEP-DOE AMIP-II reanalysis (R-2). Bulletin of the American Meteorological Society . , 2002 .
[109] J. Houghton,et al. Climate change 2001 : the scientific basis , 2001 .
[110] R. Voss,et al. Long-term climate changes due to increased CO2 concentration in the coupled atmosphere-ocean general circulation model ECHAM3/LSG , 2001 .
[111] Joseph D. Ortiz,et al. Abrupt onset and termination of the African Humid Period:rapid climate responses to gradual insolation forcing , 2000 .
[112] Sandy P. Harrison,et al. How well can we simulate past climates? Evaluating the models using global palaeoenvironmental datasets , 2000 .
[113] R. Stothers. Climatic and Demographic Consequences of the Massive Volcanic Eruption of 1258 , 1999 .
[114] Anthony C. Hirst,et al. The Southern Ocean response to global warming in the CSIRO coupled ocean-atmosphere model , 1999, Environ. Model. Softw..
[115] B. Otto‐Bliesner. El Niño/La Niña and Sahel precipitation during the Middle Holocene , 1999 .
[116] C. Torrence,et al. A Practical Guide to Wavelet Analysis. , 1998 .
[117] Syukuro Manabe,et al. Multiple-Century Response of a Coupled Ocean-Atmosphere Model to an Increase of Atmospheric Carbon Dioxide , 1994 .