Andrews, T., Gregory, J. M., and Webb, M. J.: The Dependence of Radiative Forcing and Feedback on Evolving Patterns of Surface Temperature Change in Climate Models, J. Climate, 28, 1630–1648, https://doi.org/10.1175/jcli-d-14-00545.1, 2015. a
Archer, D., Eby, M., Brovkin, V., Ridgwell, A., Cao, L., Mikolajewicz, U., Caldeira, K., Matsumoto, K., Munhoven, G., Montenegro, A., and Tokos, K.: Atmospheric Lifetime of Fossil Fuel Carbon Dioxide, Annu. Rev. Earth Planet. Sci., 37, 117–134, https://doi.org/10.1146/annurev.earth.031208.100206, 2009. a
Bathiany, S., Claussen, M., Brovkin, V., Raddatz, T., and Gayler, V.: Combined biogeophysical and biogeochemical effects of large-scale forest cover changes in the MPI earth system model, Biogeosciences, 7, 1383–1399, https://doi.org/10.5194/bg-7-1383-2010, 2010. a
Bischoff, T. and Schneider, T.: Energetic Constraints on the Position of the Intertropical Convergence Zone, J. Climate, 27, 4937–4951, 2014. a, b
Block, K. and Mauritsen, T.: Forcing and feedback in the MPI-ESM-LR coupled model under abruptly quadrupled CO2, J. Adv. Model. Earth Syst., 5, 676–691, https://doi.org/10.1002/jame.20041, 2013. a
Breitbarth, E., Oschlies, A., and LaRoche, J.: Physiological constraints on the global distribution of Trichodesmium – effect of temperature on diazotrophy, Biogeosciences, 4, 53–61, https://doi.org/10.5194/bg-4-53-2007, 2007. a
Broecker, W.: The great ocean conveyor, Oceanography, 4, 79–89, 1991. a
Broecker, W.: Thermohaline circulation, the Achilles heel of our climate system: Will man-made CO2 upset the current balance?, Science, 278, 1582–1588, https://doi.org/10.1126/science.278.5343.1582, 1997. a
Chiang, J. C. H., Biasutti, M., and Battisti, D. S.: Sensitivity of the Atlantic Intertropical Convergence Zone to Last Glacial Maximum boundary conditions, Paleoceanography, 18, 1094, https://doi.org/10.1029/2003PA000916, 2003. a
Claussen, M.: Late Quaternary vegetation-climate feedbacks, Clim. Past, 5, 203–216, https://doi.org/10.5194/cp-5-203-2009, 2009. a
Eyring, V., Bony, S., Meehl, G. A., Senior, C. A., Stevens, B., Stouffer, R. J., and Taylor, K. E.: Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization, Geosci. Model Dev., 9, 1937–1958, https://doi.org/10.5194/gmd-9-1937-2016, 2016. a
Frierson, D. M. W., Hwang, Y.-T., Fučkar, N. S., Seager, R., Kang, S. M., Donohoe, A., Maroon, E. A., Liu, X., and Battisti, D. S.: Contribution of ocean overturning circulation to tropical rainfall peak in the Northern Hemisphere, Nat. Geosci., 6, 940–944, 2013. a
Giorgetta, M., Roeckner, E., Mauritsen, T., Bader, J., Crueger, T. M. E., Rast, S., Kornblueh, L., Schmidt, H., Kinne, S., Hohenegger, C., Möbis, B., Krismer, T., Wieners, K.-H., and Stevens, B.: The atmospheric general circulation model ECHAM6 – Model description, Tech. Rep. 135, Max-Planck-Institut für Meteorologie, Hamburg, https://doi.org/10.17617/2.1810480, 2013. a
Hadley, G.: Concerning the cause of the general trade-winds: By Geo. Hadley, Esq; FRS, The Royal Society Publishing, 39, 58–62, https://doi.org/10.1098/rstl.1735.0014, 1735. a
Hoskins, B. J. and Hodges, K. I.: New perspectives on the Northern Hemisphere winter storm tracks, J. Atmos. Sci., 59, 1041–1061, 2002. a
Hutchins, D. A. and Fu, F.: Microorganisms and ocean global change, Nat. Microbiol., 2, 17058, https://doi.org/10.1038/nmicrobiol.2017.58, 2017. a
Ilyina, T., Six, K., Segschneider, J., Maier-Reimer, E., Li, H., and Nunez-Riboni, I.: Global ocean biogeochemistry model HAMOCC: Model architecture and performance as component of the MPI-Earth System Model in different CMIP5 experimental realizations, J. Adv. Model. Earth Syst., 5, 1–29, https://doi.org/10.1029/2012MS000178, 2013. a
Jungclaus, J. H., Fischer, N., Haak, H., Lohmann, K., Marotzke, J., Matei, D., Mikolajewicz, U., Notz, D., and von Storch, J. S.: Characteristics of the ocean simulations in the Max Planck Institute Ocean Model (MPIOM) the ocean component of the MPI-Earth system model, J. Adv. Model. Earth Syst., 5, 422–446, https://doi.org/10.1002/jame.20023, 2013. a
Kamphuis, V., Huisman, S. E., and Dijkstra, H. A.: The global ocean circulation on a retrograde rotating earth, Clim. Past, 7, 487–499, https://doi.org/10.5194/cp-7-487-2011, 2011. a, b, c, d, e, f, g
Kang, S. M., Held, I. M., Frierson, D. M. W., and Zhao, M.: The Response of the ITCZ to Extratropical Thermal Forcing: Idealized Slab-Ocean Experiments with a GCM, J. Climate, 21, 3521–3532, 2008. a, b, c
Kang, S. M., Frierson, D. M. W., and Held, I. M.: The Tropical Response to Extratropical Thermal Forcing in an Idealized GCM: The Importance of Radiative Feedbacks and Convective Parameterization, J. Atmos. Sci., 66, 2812–2827, 2009. a
Kaspi, Y. and Schneider, T.: Winter cold of eastern continental boundaries induced by warm ocean waters, Nature, 471, 621–624, 2011. a
Keith, D. W.: Meridional energy transport: uncertainty in zonal means, Tellus A, 47, 30–44, https://doi.org/10.3402/tellusa.v47i1.11492, 1995. a
Köppen, W.: Die Klimate der Erde: Grundriss der Klimakunde, Walter de Gruyter & Company, Berlin, 1923. a, b
Li, C., von Storch, J.-S., and Marotzke, J.: Deep-ocean heat uptake and equilibrium climate response, Clim. Dynam., 40, 1071–1086, https://doi.org/10.1007/s00382-012-1350-z, 2013. a, b
Mauritsen, T., Bader, J., Becker, T., Behrens, J., Bittner, M., Brokopf, R., Brovkin, V., Claussen, M., Crueger, T., Esch, M., Fast, I., Fiedler, S., Popke, D., Gayler, V., Giorgetta, M., Goll, D., Haak, H., Hagemann, S., Hedemann, C., Hohenegger, C., Ilyina, T., Jahns, T., Jimenez Cuesta de la Otero, D., Jungclaus, J., Kleinen, T., Kloster, S., Kracher, D., Kinne, S., Kleberg, D., Lasslop, G., Kornblueh, L., Marotzke, J., Matei, D., Meraner, K., Mikolajewicz, U., Modali, K., Möbis, B., Müller, W., Nabel, J., Nam, C., Notz, D., Nyawira, S., Paulsen, H., Peters, K., Pincus, R., Pohlmann, H., Pongratz, J., Popp, M., Raddatz, T., Rast, S., Redler, R., Reick, C., Rohrschneider, T., Schemann, V., Schmidt, H., Schnur, R., Schulzweida, U., Six, K., Stein, L., Stemmler, I., Stevens, B., von Storch, J., Tian, F., Voigt, A., de Vrese, P., Wieners, K.-H., Wilkenskjeld, S., Roeckner, E., and Winkler, A.: Developments in the MPI-M Earth System Model version 1.2 (MPI-ESM1.2) and its response to increasing CO2, J. Adv. Model. Earth Syst., in review, 2018. a
Moore, J. K. and Braucher, O.: Sedimentary and mineral dust sources of dissolved iron to the world ocean, Biogeosciences, 5, 631–656, https://doi.org/10.5194/bg-5-631-2008, 2008. a
MPI: Model distribution: https://www.mpimet.mpg.de/en/science/models/license/, last accessed: 9 October 2018. a
Munzar, J.: Alexander von Humboldt and his isotherms, Weather, 22, 360–363, 2012. a
Notz, D., Haumann, F. A., Haak, H., Jungclaus, J. H., and Marotzke, J.: Arctic sea-ice evolution as modeled by Max Planck Institute for Meteorology's Earth system model, J. Adv. Model. Earth Syst., 5, 173–194, https://doi.org/10.1002/jame.20016, 2013. a
Paulsen, H., Ilyina, T., Six, K., and Stemmler, I.: Incorporating a prognostic representation of marine nitrogen fixers into the global ocean biogeochemical model HAMOCC, J. Adv. Model. Earth Syst., 9, 438–464, https://doi.org/10.1002/2016MS000737, 2017. a
Philander, S. G. H., Gu, D., Lambert, G., Li, T., Halpern, D., Lau, N. C., and Pacanowski, R. C.: Why the ITCZ Is Mostly North of the Equator, J. Climate, 9, 2958–2972, 1996. a, b, c
Rae, J. W. B. and Broecker, W.: What Fraction of the Pacific and Indian Oceans' Deep Water is formed in the North Atlantic?, Biogeosciences Discuss., https://doi.org/10.5194/bg-2018-8, in review, 2018. a
Reick, C. H., Raddatz, T., Brovkin, V., and Gayler, V.: Representation of natural and anthropogenic land cover change in MPI-ESM, J. Adv. Model. Earth Syst., 5, 459–482, https://doi.org/10.1002/jame.20022, 2013. a
Rodwell, M. J. and Hoskins, B. J.: Monsoons and the dynamics of deserts, Q. J. Roy. Meteorol. Soc., 122, 1385–1404, 1996. a, b
Seager, R., Battisti, D. S., Yin, J., Gordon, N., Naik, N., Clement, A. C., and Cane, M. A.: Is the Gulf Stream responsible for Europe's mild winters?, Q. J. Roy. Meteorol. Soc., 128, 2563–2586, 2002. a
Smith, R. S.: The FAMOUS climate model (versions XFXWB and XFHCC): description update to version XDBUA, Geosci. Model Dev., 5, 269–276, https://doi.org/10.5194/gmd-5-269-2012, 2012. a
Smith, R. S., Gregory, J. M., Thorpe, R. B., and Rodriguez, J.: Response of the meridional overturning circulation in an idealised reverse world experiment, in: EGU General Assembly, session CL26 poster; Ref. No.: EGU2008-A-06893, EGU, 13–18 April 2008, Vienna, Austria, 2008. a, b, c, d, e
Sohm, J. A., Webb, E. A., and Capone, D. G.: Emerging patterns of marine nitrogen fixation, Nat. Rev. Microbiol., 9, 499–508, https://doi.org/10.1038/nrmicro2594, 2011. a, b
Stephens, G. L., Juilin, L., Wild, M., Clayson, C. A., Loeb, N. G., Kato, S., L'Ecuyer, T., Stackhouse Jr., P. W., and Andrews, T.: The energy blance of the Earth's climate system, Nat. Geosci., 5, 691–696, 2012. a
Stevens, B. and Schwartz, S. E.: Observing and Modeling Earth's Energy Flows, Surv. Geophys., 33, 779–816, 2012. a, b
Stevens, B., Giorgetta, M., Esch, M., Mauritsen, T., Crueger, T., Rast, S., Salzmann, M., Schmidt, H., Bader, J., Block, K., Brokopf, R., Fast, I., Kinne, S., Kornblueh, L., Lohmann, U., Pincus, R., Reichler, T., and Roeckner, E.: Atmospheric component of the MPI-M Earth System Model: ECHAM6, J. Adv. Model. Earth Syst., 5, 146–172, 2013. a
Stommel, H.: Thermohaline Convection with Two Stable Regimes of Flow, Tellus, 13, 224–230, https://doi.org/10.1111/j.2153-3490.1961.tb00079.x, 1961. a
Vamborg, F., Brovkin, V., and Claussen, M.: The effect of dynamic background albedo scheme on Sahel/Sahara precipitation during the Mid-Holocene, Clim. Past, 7, 117–131, https://doi.org/10.5194/cp-7-117-2011, 2011. a
von Humboldt, A.: Des Lignes Isothermes, Cambridge University Press, Paris, 1817. a
Wallace, J. M., Mitchell, T. P., and Deser, C.: The Influence of Sea-Surface Temperature on Surface Wind in the Eastern Equatorial Pacific: Seasonal and Interannual Variability, J. Climate, 2, 1492–1499, 1989. a, b, c
Warren, B. A.: Why is no deep water formed in the North Pacific?, J. Mar. Res., 41, 327–347, https://doi.org/10.1357/002224083788520207, 1983. a, b
WDC Climate: The climate of a retrograde rotating earth (data): https://cera-www.dkrz.de/WDCC/ui/cerasearch/entry?acronym=DKRZ_LTA_110_ds00001, last access: 9 October 2018. a
Zelinka, M. D. and Hartmann, D. L.: Why is longwave cloud feedback positive?, J. Geophys. Res.-Atmos., 115, D16117, https://doi.org/10.1029/2010JD013817, 2010. a
Zhou, C., Zelinka, M. D., and Klein, S. A.: Impact of decadal cloud variations on the Earth's energy budget, Nat. Geosci., 9, 871–874, https://doi.org/10.1038/ngeo2828, 2016. a
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