Articles | Volume 10, issue 2
https://doi.org/10.5194/cp-10-697-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-10-697-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
03 Apr 2014
Research article |
| 03 Apr 2014
The faint young Sun problem revisited with a 3-D climate–carbon model – Part 1
G. Le Hir
IPGP, Institut de Physique du Globe de Paris, Sorbonne Paris cité, Université Paris Diderot, UMR7154, 75005, France
Y. Teitler
IPGP, Institut de Physique du Globe de Paris, Sorbonne Paris cité, Université Paris Diderot, UMR7154, 75005, France
now at: Centre for Exploration Targeting, University of Western Australia, Crawley, Australia
F. Fluteau
IPGP, Institut de Physique du Globe de Paris, Sorbonne Paris cité, Université Paris Diderot, UMR7154, 75005, France
Y. Donnadieu
LSCE, CNRS-CEA-UVSQ, 91191 Gif-sur-Yvette, France
P. Philippot
IPGP, Institut de Physique du Globe de Paris, Sorbonne Paris cité, Université Paris Diderot, UMR7154, 75005, France
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A new version (v7) of the numerical model GEOCLIM is presented here. GEOCLIM models the evolution of ocean and atmosphere chemical composition on multi-million years timescale, including carbon and oxygen cycles, CO2 and climate. GEOCLIM is associated to a climate model, and a new procedure to link the climate model to GEOCLIM is presented here. GEOCLIM is applied here to investigate the evolution of ocean oxygenation following Earth's orbital parameter variations, around 94 million years ago.
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The Asian monsoons onset has been suggested to be as early as 40 Ma, in a palaeogeographic and climatic context very different from modern conditions. We test the likeliness of an early monsoon onset through climatic modelling. Our results reveal a very arid central Asia and several regions in India, Myanmar and eastern China experiencing highly seasonal precipitations. This suggests that monsoon circulation is not paramount in triggering the highly seasonal patterns recorded in the fossils.
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Daniel J. Lunt, Fran Bragg, Wing-Le Chan, David K. Hutchinson, Jean-Baptiste Ladant, Polina Morozova, Igor Niezgodzki, Sebastian Steinig, Zhongshi Zhang, Jiang Zhu, Ayako Abe-Ouchi, Eleni Anagnostou, Agatha M. de Boer, Helen K. Coxall, Yannick Donnadieu, Gavin Foster, Gordon N. Inglis, Gregor Knorr, Petra M. Langebroek, Caroline H. Lear, Gerrit Lohmann, Christopher J. Poulsen, Pierre Sepulchre, Jessica E. Tierney, Paul J. Valdes, Evgeny M. Volodin, Tom Dunkley Jones, Christopher J. Hollis, Matthew Huber, and Bette L. Otto-Bliesner
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A. Pohl, Y. Donnadieu, G. Le Hir, J.-F. Buoncristiani, and E. Vennin
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J.-B. Ladant, Y. Donnadieu, and C. Dumas
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P. Yiou, M. Boichu, R. Vautard, M. Vrac, S. Jourdain, E. Garnier, F. Fluteau, and L. Menut
Clim. Past, 10, 797–809, https://doi.org/10.5194/cp-10-797-2014, https://doi.org/10.5194/cp-10-797-2014, 2014
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Subject: Climate Modelling | Archive: Modelling only | Timescale: Pre-Cenozoic
Diagnosing the controls on desert dust emissions through the Phanerozoic
Exploring the mechanisms of Devonian oceanic anoxia: impact of ocean dynamics, palaeogeography and orbital forcing
Effects of ozone levels on climate through Earth history
Climate and ocean circulation in the aftermath of a Marinoan snowball Earth
Deep ocean temperatures through time
The Pliocene Model Intercomparison Project Phase 2: large-scale climate features and climate sensitivity
Paleogeographic controls on the evolution of Late Cretaceous ocean circulation
Stripping back the modern to reveal the Cenomanian–Turonian climate and temperature gradient underneath
Diminished greenhouse warming from Archean methane due to solar absorption lines
The initiation of Neoproterozoic "snowball" climates in CCSM3: the influence of paleocontinental configuration
Albedo and heat transport in 3-D model simulations of the early Archean climate
Sea-ice dynamics strongly promote Snowball Earth initiation and destabilize tropical sea-ice margins
The Aptian evaporites of the South Atlantic: a climatic paradox?
The initiation of modern soft and hard Snowball Earth climates in CCSM4
Initiation of a Marinoan Snowball Earth in a state-of-the-art atmosphere-ocean general circulation model
Clouds and the Faint Young Sun Paradox
Model-dependence of the CO2 threshold for melting the hard Snowball Earth
Yixuan Xie, Daniel J. Lunt, and Paul J. Valdes
Clim. Past, 20, 2561–2585, https://doi.org/10.5194/cp-20-2561-2024, https://doi.org/10.5194/cp-20-2561-2024, 2024
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Desert dust plays a crucial role in the climate system; while it is relatively well studied for the present day, we still lack knowledge on how it was in the past and on its underlying mechanism in the multi-million-year timescale of Earth’s history. For the first time, we simulate dust emissions using the newly developed DUSTY1.0 model over the past 540 million years with a temporal resolution of ~5 million years. We find that palaeogeography is the primary control of these variations.
Justin Gérard, Loïc Sablon, Jarno J. C. Huygh, Anne-Christine Da Silva, Alexandre Pohl, Christian Vérard, and Michel Crucifix
EGUsphere, https://doi.org/10.5194/egusphere-2024-1983, https://doi.org/10.5194/egusphere-2024-1983, 2024
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We used cGENIE, a climate model, to explore how changes in continental configuration, CO2 levels, and orbital configuration affect ocean oxygen levels during the Devonian period (419–359 million years ago). Key factors contributing to ocean anoxia were identified, highlighting the influence of continental configurations, atmospheric conditions, and orbital changes. Our findings offer new insights into the causes and prolonged durations of Devonian ocean anoxic events.
Russell Deitrick and Colin Goldblatt
Clim. Past, 19, 1201–1218, https://doi.org/10.5194/cp-19-1201-2023, https://doi.org/10.5194/cp-19-1201-2023, 2023
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Prior to 2.5 billion years ago, ozone was present in our atmosphere only in trace amounts. To understand how climate has changed in response to ozone build-up, we have run 3-D climate simulations with different amounts of ozone. We find that Earth's surface is about 3 to 4 °C degrees cooler with low ozone. This is caused by cooling of the upper atmosphere, where ozone is a warming agent. Its removal causes the upper atmosphere to become drier, weakening the greenhouse warming by water vapor.
Lennart Ramme and Jochem Marotzke
Clim. Past, 18, 759–774, https://doi.org/10.5194/cp-18-759-2022, https://doi.org/10.5194/cp-18-759-2022, 2022
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After the Marinoan snowball Earth, the climate warmed rapidly due to enhanced greenhouse conditions, and the freshwater inflow of melting glaciers caused a strong stratification of the ocean. Our climate simulations reveal a potentially only moderate global temperature increase and a break-up of the stratification within just a few thousand years. The findings give insights into the environmental conditions relevant for the geological and biological evolution during that time.
Paul J. Valdes, Christopher R. Scotese, and Daniel J. Lunt
Clim. Past, 17, 1483–1506, https://doi.org/10.5194/cp-17-1483-2021, https://doi.org/10.5194/cp-17-1483-2021, 2021
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Deep ocean temperatures are widely used as a proxy for global mean surface temperature in the past, but the underlying assumptions have not been tested. We use two unique sets of 109 climate model simulations for the last 545 million years to show that the relationship is valid for approximately the last 100 million years but breaks down for older time periods when the continents (and hence ocean circulation) are in very different positions.
Alan M. Haywood, Julia C. Tindall, Harry J. Dowsett, Aisling M. Dolan, Kevin M. Foley, Stephen J. Hunter, Daniel J. Hill, Wing-Le Chan, Ayako Abe-Ouchi, Christian Stepanek, Gerrit Lohmann, Deepak Chandan, W. Richard Peltier, Ning Tan, Camille Contoux, Gilles Ramstein, Xiangyu Li, Zhongshi Zhang, Chuncheng Guo, Kerim H. Nisancioglu, Qiong Zhang, Qiang Li, Youichi Kamae, Mark A. Chandler, Linda E. Sohl, Bette L. Otto-Bliesner, Ran Feng, Esther C. Brady, Anna S. von der Heydt, Michiel L. J. Baatsen, and Daniel J. Lunt
Clim. Past, 16, 2095–2123, https://doi.org/10.5194/cp-16-2095-2020, https://doi.org/10.5194/cp-16-2095-2020, 2020
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The large-scale features of middle Pliocene climate from the 16 models of PlioMIP Phase 2 are presented. The PlioMIP2 ensemble average was ~ 3.2 °C warmer and experienced ~ 7 % more precipitation than the pre-industrial era, although there are large regional variations. PlioMIP2 broadly agrees with a new proxy dataset of Pliocene sea surface temperatures. Combining PlioMIP2 and proxy data suggests that a doubling of atmospheric CO2 would increase globally averaged temperature by 2.6–4.8 °C.
Jean-Baptiste Ladant, Christopher J. Poulsen, Frédéric Fluteau, Clay R. Tabor, Kenneth G. MacLeod, Ellen E. Martin, Shannon J. Haynes, and Masoud A. Rostami
Clim. Past, 16, 973–1006, https://doi.org/10.5194/cp-16-973-2020, https://doi.org/10.5194/cp-16-973-2020, 2020
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Understanding of the role of ocean circulation on climate is contingent on the ability to reconstruct its modes and evolution. Here, we show that earth system model simulations of the Late Cretaceous predict major changes in ocean circulation as a result of paleogeographic and gateway evolution. Comparisons of model results with available data compilations demonstrate reasonable agreement but highlight that various plausible theories of ocean circulation change coexist during this period.
Marie Laugié, Yannick Donnadieu, Jean-Baptiste Ladant, J. A. Mattias Green, Laurent Bopp, and François Raisson
Clim. Past, 16, 953–971, https://doi.org/10.5194/cp-16-953-2020, https://doi.org/10.5194/cp-16-953-2020, 2020
Short summary
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To quantify the impact of major climate forcings on the Cretaceous climate, we use Earth system modelling to progressively reconstruct the Cretaceous state by changing boundary conditions one by one. Between the preindustrial and the Cretaceous simulations, the model simulates a global warming of more than 11°C. The study confirms the primary control exerted by atmospheric CO2 on atmospheric temperatures. Palaeogeographic changes represent the second major contributor to the warming.
B. Byrne and C. Goldblatt
Clim. Past, 11, 559–570, https://doi.org/10.5194/cp-11-559-2015, https://doi.org/10.5194/cp-11-559-2015, 2015
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High methane concentrations are thought to have helped sustain warm surface temperatures on the early Earth (~3 billion years ago) when the sun was only 80% as luminous as today. However, radiative transfer calculations with updated spectral data show that methane is a stronger absorber of solar radiation than previously thought. In this paper we show that the increased solar absorption causes a redcution in the warming ability of methane in the Archaean atmosphere.
Y. Liu, W. R. Peltier, J. Yang, and G. Vettoretti
Clim. Past, 9, 2555–2577, https://doi.org/10.5194/cp-9-2555-2013, https://doi.org/10.5194/cp-9-2555-2013, 2013
H. Kienert, G. Feulner, and V. Petoukhov
Clim. Past, 9, 1841–1862, https://doi.org/10.5194/cp-9-1841-2013, https://doi.org/10.5194/cp-9-1841-2013, 2013
A. Voigt and D. S. Abbot
Clim. Past, 8, 2079–2092, https://doi.org/10.5194/cp-8-2079-2012, https://doi.org/10.5194/cp-8-2079-2012, 2012
A.-C. Chaboureau, Y. Donnadieu, P. Sepulchre, C. Robin, F. Guillocheau, and S. Rohais
Clim. Past, 8, 1047–1058, https://doi.org/10.5194/cp-8-1047-2012, https://doi.org/10.5194/cp-8-1047-2012, 2012
J. Yang, W. R. Peltier, and Y. Hu
Clim. Past, 8, 907–918, https://doi.org/10.5194/cp-8-907-2012, https://doi.org/10.5194/cp-8-907-2012, 2012
A. Voigt, D. S. Abbot, R. T. Pierrehumbert, and J. Marotzke
Clim. Past, 7, 249–263, https://doi.org/10.5194/cp-7-249-2011, https://doi.org/10.5194/cp-7-249-2011, 2011
C. Goldblatt and K. J. Zahnle
Clim. Past, 7, 203–220, https://doi.org/10.5194/cp-7-203-2011, https://doi.org/10.5194/cp-7-203-2011, 2011
Y. Hu, J. Yang, F. Ding, and W. R. Peltier
Clim. Past, 7, 17–25, https://doi.org/10.5194/cp-7-17-2011, https://doi.org/10.5194/cp-7-17-2011, 2011
Cited articles
Abbot, D. S., Voigt, A., Branson, M., Pierrehumbert, R. T., Pollard, D., Le Hir, G., and Koll, D. D. B.: Clouds and snowball Earth deglaciation, Geophys. Res. Lett., 39, L20711, https://doi.org/10.1029/2012GL052861, 2012.
Andreae, M. O. and Rosenfeld, D.: Aerosol–cloud–precipitation interactions. Part 1. The nature and sources of cloud-active aerosols, Earth-Sci. Rev., 89, 13–41, https://doi.org/10.1016/j.earscirev.2008.03.001, 2008.
Boucher, O., Le Treut, H., and Baker, M. B.: Precipitation and radiation modeling in a general circulation model: Introduction of cloud microphysical processes, J. Geophys. Res., 100, 16395–16414, https://doi.org/10.1029/95JD01382, 1995.
Bréon, F. M., Tanré, D., and Generoso, S.: Aerosol Effect on Cloud Droplet Size Monitored from Satellite, Science, 295, 834–838, https://doi.org/10.1126/science.1066434, 2002.
Catling, D. C., Claire, M. W., and Zahnle, K. J.: Anaerobic methanotrophy and the rise of atmospheric oxygen, Phil. Trans. R. Soc., 365, 1867–1888, https://doi.org/10.1098/rsta.2007.2047, 2007.
Charlson, R. J., Lovelock, J. E., Andreae, M. O., and Warren, S. G.: Oceanic Phytoplankton, atmospheric sulfur, cloud albedo and climate, Nature, 326, 655–661, 1987.
Charney, B., Forget, F., Wordworth, R., Leconte, J., Millour, E., Codron, F., and Spiga, A.: Exploring the faint young Sun problem and the possible climates of the Archean Earth with a 3-D GCM, J. Geophys. Res., 118, 10414–10431, https://doi.org/10.1002/jgrd.50808, 2013.
Dauphas, N. and Kasting, J. F.: Low pCO2 in the pore water, not in the Archean air, Nature, 474, E2–E3, https://doi.org/10.1038/nature09960, 2011.
Driese, S. G., Jirsa, M. A., Ren, M., Brantley, S. L., Sheldon, N. D., Parker, D., and Schmitz, M.: Neoarchean paleoweathering of tonalite and metabasalt: implicationsq for reconstructions of 2.69 Ga early terrestrial ecosystems and paleoatmospheric chemistry, Precambrian Res., 187, 1–17, https://doi.org/10.1016/j.precamres.2011.04.003, 2011.
Farquhar, J., Airieau, S., and Thiemens, M. H.: Observation of wavelength-sensitive mass-independent sulfur isotope effects during SO2 photolysis: Implications for the early atmosphere, J. Geophy. Res.-Planets, 106, 32829–32839, 2001.
Feulner, G.: The faint young sun problem, Rev. Geophys., 50, RG2006, https://doi.org/10.1029/2011RG000375, 2012.
Foriel, J., Philippot, P., Rey, P., Somogyi, A., Banks, D., and Menez, B.: Biological control of Cl/Br and low sulfate concentration in a 3.5-Gyr-old seawater from North Pole, Western Australia, Earth Planet. Sci. Lett., 228, 451–463, 2004.
Godderis, Y. and Veizer, J.: Tectonic control of chemical and isotopic composition of ancient oceans: the impact of continental growth, Am. J. Sci., 300, 434–461, 2000.
Goldblatt, C. and Zahnle, K. J.: Faint Young Sun Paradox remains, Nature, 474, E1, https://doi.org/10.1038/nature09961, 2011a.
Goldblatt, C. and Zahnle, K. J.: Clouds and the Faint Young Sun Paradox, Clim. Past, 7, 203–220, https://doi.org/10.5194/cp-7-203-2011, 2011b.
Goldblatt, C., Claire, M. W., Lenton, T. M., Matthews, A. J., Watson. A. J., and Zahnle, K. J.: Nitrogen-enhanced greenhouse warming on early Earth, Nat. Geosci., 2, 891–896, https://doi.org/10.1038/NGEO692, 2009.
Gough, D. O.: Solar interior structure and luminosity variations, Sol. Phys., 74, 21–34, 1981.
Hack, J. J.: Sensitivity of the simulated climate to a diagnostic formulation for cloud liquid water, J. Climate, 11, 1497–1515, 1998.
Halevy, I., Pierrehumbert, R. T., and Schrag, D. P.: Radiative transfer in CO2-rich paleoatmospheres, J. Geophys. Res., 114, D18112, https://doi.org/10.1029/2009JD011915, 2009.
Hansen, J., Sato, M., and Ruedy, R.: Radiative Forcing and climate response, J. Geophys. Res., 102, 6831–6864, 1997.
Haqq-Misra, J. D., Domagal-Goldman, S. D., Kasting, P. J., and Kasting, J. F.: A revised, hazy methane greenhouse for the archean Earth, Astrobiology, 8, 1127–1137, 2008.
Jacob, R.: Low frequency variability in a simulated atmosphere ocean system, PhD Thesis, University of Wisconsin-Madison, 1997–310, 1997.
Jenkins, G. S.: The effects of reduced land fraction and solar forcing on the general circulation results from the NCAR CCM, Glob. Planet. Change, 7, 321–333, 1993a.
Jenkins, G. S.: A General Circulation Model Study of the Effects of Faster Rotation Rate, Enhanced CO2 Concentration, and Reduced Solar Forcing' Implications for the Faint Young Sun Paradox, J. Geophys. Res., 98, 20803–20811, 1993b.
Jenkins, G. S., Marshall, H. G., and Kuhn, W. R.: Precambrian climate – the effects of land area and Earth's rotation rate, J. Geophys. Res.-Atmos., 98, 8785–8791, https://doi.org/10.1029/93JD00033, 1993.
Kasting, J. F.: The evolution of the prebiotic atmosphere, Origins Life Evol. B., 14, 75–82, 1984.
Kasting, J. F.: Theoretical constraints on oxygen and carbon-dioxide concentrations in the Pre-cambrian atmosphere, Precambrian Res., 34, 205–229, 1987.
Kasting, J. F.: Early Earth faint young sun redux, Nature, 464, 687–689, 2010.
Kiehl, J. T. and Dickinson, R. E.: A study of the radiative effects of enhanced atmospheric CO2 and CH4 on early Earth surface temperatures, J. Geophys. Res.-Atmos., 92, 2991–2998, 1987.
Kienert, H., Feulner, G., and Petoukhov, V.: Faint young sun problem more severe due to ice-albedo feedback and higher rotation rate of the early Earth, Geophys. Res. Lett., 39, L23710, https://doi.org/10.1029/2012GL054381, 2012.
Kienert, H., Feulner, G., and Petoukhov, V.: Albedo and heat transport in 3-D model simulations of the early Archean climate, Clim. Past, 9, 1841–1862, https://doi.org/10.5194/cp-9-1841-2013, 2013.
Knauth, L. P.: Temperature and salinity history of the Precambrian ocean: implications for the course of microbial evolution, Palaeogeogr. Palaeocl., 219, 53–69, 2005.
Kump, L. R. and Pollard, D.: Amplification of cretaceous warmth by biological cloud feedbacks, Science, 320, 195–195, 2008.
Kunze, M., Godolt, M., Langematz, U., Grenfell, J. L., Hamann-Reinus, A., and Rauer, H.: Investigating the early Earth faint young Sun problem with a general circulation model, Planet. Space Sci., https://doi.org/10.1016/j.pss.2013.09.011, in press, 2014.
Le Hir, G., Donnadieu, Y., Krinner, G., and Ramstein, G.: Toward the snowball earth deglaciation, Clim. Dynam., 35, 285–297, 2010.
Lowe, D. R. and Tice, M. M.: Tectonic controls on atmospheric, climatic, and biological evolution 3.5–2.5 Ga, Precambrian Res., 158, 177–197, 2007.
MacKay, R. M. and Khalil, M. A. K.: Theory and Development of a One Dimensional Time Dependant Radiative Convective Climate Model, Chemosphere, 22, 383–417, 1991.
Millero, F. J. and Poisson, A.: International one-atmosphere equation of state of seawater, Deep-Sea Res. Pt. I, 28, 625–629, 1981.
Pavlov, A. A., Kasting, J. F., Brown, L. L., Rages, K. A., and Freedman, R.: Greenhouse warming by CH4 in the atmosphere of early Earth, J. Geophys. Res.-Planets, 105, 11981–11990, 2000.
Penner, J. E., Quaas, J., Storelvmo, T., Takemura, T., Boucher, O., Guo, H., Kirkevåg, A., Kristjánsson, J. E., and Seland, Ø.: Model intercomparison of indirect aerosol effects, Atmos. Chem. Phys., 6, 3391–3405, https://doi.org/10.5194/acp-6-3391-2006, 2006.
Petoukhov, V., Ganopolski, A., Brovkin, V., Claussen, M., Eliseev, A., Kubatzki, C., and Rahmstorf, S.: CLIMBER-2: a climate system model of intermediate complexity. Part I: model description and performance for present climate, Clim. Dynam. 16, 1–17, https://doi.org/10.1007/PL00007919, 2000.
Pesonen, L. J., Elming, S. A, Mertanen, S., Pisarevsky, S., D'Agrella-Filho, M. S., Meert, J. G., Schmidt, P. W., Abrahamsen, N., and Bylund, G.: Palaeomagnetic configuration of continents during the Proterozoic, Tectonophysics, 375, 289–324, 2003.
Pierrehumbert, R. T.: High levels of atmospheric carbon dioxide necessary for the termination of global glaciation, Nature, 429, 646–649, 2004.
Pierrehumbert, R. T.: Principles of Planetary Climate, Cambridge University Press, 652 pp., 2010.
Pierrehumbert, R. T., Abbot, D. S., Voigt., A., and Koll, D.: Climate of the Neoproterozoic Annual, Rev. Earth Planet. Sci., 39, 417–460, https://doi.org/10.1146/annurev-earth-040809-152447, 2011.
Reinhard, C. T. and Planavsky, N. J.: Mineralogical constraints on Precambrian pCO2, Nature, 474, E1–E2, https://doi.org/10.1038/nature09959, 2011.
Rosing, M. T., Bird, D. K., Sleep, N. H., and Bjerrum, C. J.: No climate paradox under the faint early Sun, Nature, 464, 744–747, https://doi.org/10.1038/nature08955, 2010.
Rye, R., Kuo, P. H., and Holland, H. D.: Atmospheric carbon-dioxide concentrations before 2.2-billion years ago, Nature, 378, 603–605, 1995.
Sagan, C. and Mullen, G.: Earth and Mars – evolution of atmospheres and surface tempera-tures, Science, 177, 52–56, https://doi.org/10.1126/science.177.4043.52, 1972.
Schatten, K. H. and Endal, A. S.: The faint young Sun climate paradox – volcanic influence, Geophys. Res. Lett., 9, 1309–1311, https://doi.org/10.1029/GL009i012p01309, 1982.
Sheldon, N. D.: Precambrian paleosols and atmospheric CO2 levels, Precambrian Res., 147, 148–155, 2006.
Slingo, A.: A GCM parameterization for the shortwave radiative properties of water clouds, J. Atmos. Sci., 46, 1419–1427, 1989.
Stevens, B. and Bony, S.: What Are Climate Models Missing?, Science, 340, 1053–1054, https://doi.org/10.1126/science.1237554, 2013.
Voigt, A. and Abbot, D. S.: Sea-ice dynamics strongly promote Snowball Earth initiation and destabilize tropical sea-ice margins, Clim. Past, 8, 2079–2092, https://doi.org/10.5194/cp-8-2079-2012, 2012.
von Paris, P., Rauer, H., Grenfell, J. L., Patzer, B., Hedelt, P., Stracke, B., Trautmann, T., and Schreier, F.: Warming the early earth-CO2 reconsidered, Planet. Space Sci., 56, 1244–1259 https://doi.org/10.1016/j.pss.2008.04.008, 2008.
Walker, J. C. G.: Climatic factors on the Archean Earth, Palaeogr. Palaeocl., 40, 1–11, https://doi.org/10.1016/0031-0182(82)90082-7, 1982.
Walker, J. C. G., Hays, P. B., and Kasting, J. F.: A Negative Feedback Mechanism For The Long-Term Stabilization of Earth's Surface-Temperature, J. Geophys. Res.-Ocean. Atmos., 86, 9776–9782, 1981.
Wang, W. and Stone, P. H.: Effect of Ice-Albedo Feedback on Global Sensitivity in a One-Dimensional Radiative-Convective Climate Model, J. Atmophs. Sci., 37, 545–552, 1980.
Warren, S. G., Brandt, R. E., Grenfell, T. C., and McKay, C. P.: Snowball Earth: Ice thickness on the tropical ocean, J. Geophys. Res.-Ocean., 107, 31-1–31-18, https://doi.org/10.1029/2001JC001123, 2002.
Williams, P. D., Guilyardi, E., Madec, G., Gualdi, S., and Scoccimarro, E.: The role of mean ocean salinity in climate, Dynam. Atmos. Oceans, 49, 108–123, https://doi.org/10.1016/j.dynatmoce.2009.02.001, 2010.
Wolf, E. T. and Toon, O. B.: Hospitable Archean Climates Simulated by a General Circulation Model, Astrobiology, 13, 656–673, https://doi.org/10.1089/ast.2012.0936, 2013.
Wordsworth, R. and Pierrehumbert, R.: Hydrogen-nitrogen greenhouse warming in Earth's early atmosphere, Science, 339, 64–67, https://doi.org/10.1126/science.1225759, 2013.
