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2011 | OriginalPaper | Buchkapitel

8. Atmosphere–Ocean Interactions

verfasst von : Thomas Stocker

Erschienen in: Introduction to Climate Modelling

Verlag: Springer Berlin Heidelberg

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Abstract

Energy, momentum and matter (water, carbon, nitrogen,...) are exchanged between the ocean and the atmosphere. Most of the movements in the ocean, particularly the large-scale flow, are caused by these exchange fluxes. Consequently, they need to be reproduced in a climate model as realistically as possible. In the context of this book we will not treat micro-scale fluxes, occurring on a cm- or smaller scale. An in-depth description is provided by Kraus and Businger (1994). We will only present the parameterisations that are implemented mainly in climate models of coarse resolution. Formulations of so-called boundary layers in the atmosphere and ocean are also not discussed.

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Vorheriges Kapitel Large-Scale Circulation in the Atmosphere

Nächstes Kapitel Multiple Equilibria in the Climate System

Alley, R.B., J. Marotzke, W.D. Nordhaus, J.T. Overpeck, D.M. Peteet, R.A. Pielke Jr., R.T. Pierrehumbert, P.B. Rhines, T.F. Stocker, L.D. Talley, and J.M. Wallace (2003): Abrupt climate change. Science, 299, 2005–2010.CrossRef

Barker, S., P. Diz, M.J. Vautravers, J. Pike, G. Knorr, I.R. Hall, and W.S. Broecker (2009): Interhemispheric Atlantic seesaw response during the last deglaciation. Nature, 457, 1097–1102.CrossRef

Blunier, T. and E.J. Brook (2001): Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period. Science, 291, 109–112.CrossRef

Blunier, T., J. Chappellaz, J. Schwander, A. Dällenbach, B. Stauffer, T.F. Stocker, D. Raynaud, J. Jouzel, H.B. Clausen, C.U. Hammer, and S.J. Johnsen (1998): Asynchrony of Antarctic and Greenland climate change during the last glacial period. Nature, 394, 739–743.CrossRef

Bony, S., R. Colman, V.M. Kattsov, R.P. Allan, C.S. Bretherton, J.L. Dufresne, A. Hall, S. Hallegatte, M.M. Holland, W. Ingram, D.A. Randall, B.J. Soden, G. Tselioudis, and M.J. Webb (2006): How well do we understand and evaluate climate change feedback processes? J. Climate, 19, 3445–3482.CrossRef

Broecker, W.S. (1987): The biggest chill. Nat. Hist., 96, 74–82.

Broecker, W.S. (1997): Thermohaline circulation, the Achilles heel of our climate system: will man-made CO2 upset the current balance? Science, 278, 1582–1588.CrossRef

Broecker, W.S. (1998): Paleocean circulation during the last deglaciation: a bipolar seesaw? Paleoceanography, 13, 119–121.CrossRef

Broecker, W.S. and G.H. Denton (1989): The role of ocean-atmosphere reorganizations in glacial cycles. Geochim. Cosmochim. Ac., 53, 2465–2501.CrossRef

Broecker, W.S., D.M. Peteet, and D. Rind (1985): Does the ocean-atmosphere system have more than one stable mode of operation? Nature, 315, 21–26.CrossRef

Bryan, F. (1986): High-latitude salinity effects and interhemispheric thermohaline circulations. Nature, 323, 301–304.CrossRef

Bryan, F. (1987): Parameter sensitivity of primitive equation ocean general circulation models. J. Phys. Oceanogr., 17, 970–985.CrossRef

Bryan, K. and M.D. Cox (1967): A numerical investigation of the oceanic general circulation. Tellus, 19, 54–80.CrossRef

Budyko, M.I. (1969): The effect of solar radiation variations on the climate of the earth. Tellus, 21, 611–619.CrossRef

Cayan, D.R. (1992): Latent and Sensible Heat Flux Anomalies over the Northern Oceans: The Connection to Monthly Atmospheric Circulation. J. Climate, 5, 354–370.CrossRef

Clark, P.U., N.G. Pisias, T.F. Stocker, and A.J. Weaver (2002): The role of the thermohaline circulation in abrupt climate change. Nature, 415, 863–869.CrossRef

Colman, R. (2003): A comparison of climate feedbacks in general circulation models. Clim. Dyn., 20, 865–873.

Copenhagen Accord (2009): Document available at http://unfccc.int.

Courant, R., K. Friedrichs, and H. Lewy (1928): Über die partiellen Differenzengleichungen der mathematischen Physik. Math. Ann., 100, 32–74.CrossRef

Dansgaard, W., S.J. Johnsen, H.B. Clausen, D. Dahl-Jensen, N. Gundestrup, C.U. Hammer, and H. Oeschger (1984): North Atlantic climatic oscillations revealed by deep Greenland ice cores. In: J.E. Hansen (Editor), Climate Processes and Climate Sensitivity (Geophysical Monograph), pp. 288–298. American Geophysical Union.

Dansgaard, W., S.J. Johnsen, H.B. Clausen, D. Dahl-Jensen, N.S. Gundestrup, C.U. Hammer, C.S. Hvidberg, J.P. Steffensen, A.E. Sveinbjörnsdottir, J. Jouzel, and G. Bond (1993): Evidence for general instability of past climate from a 250-kyr ice-core record. Nature, 364, 218–220.CrossRef

Domingues, C.M., J.A. Church, N.J. White, P.J. Gleckler, S.E. Wijffels, P.M. Barker, and J.R. Dunn (2008): Improved estimates of upper-ocean warming and multi-decadal sea-level rise. Nature, 453, 1090–1093.CrossRef

Egger, J. (1997): Flux correction: Tests with a simple ocean-atmosphere model. Clim. Dyn., 13, 285–292.CrossRef

EPICA Community Members (2006): One-to-one coupling of glacial climate variability in Greenland and Antarctica. Nature, 444, 195–198.CrossRef

Ferreira, D., J. Marshall, and B. Rose (2011): Climate determinism revisited: Multiple equilibria in a complex climate model. J. Climate, 24, 992–1012.CrossRef

Ganachaud, A. and C. Wunsch (2000): Improved estimates of global ocean circulation, heat transport and mixing from hydrographic data. Nature, 408, 453–457.CrossRef

Gill, A.E. (1982): Atmosphere–Ocean Dynamics. Academic Press, 662 pp.

Haltiner, G.J. and R.T. Williams (1980): Numerical Prediction and Dynamic Meteorology. Wiley, 2 ed., 496 pp.

Haney, R.L. (1971): Surface thermal boundary condition for ocean circulation models. J. Phys. Oceanogr., 1, 241–248.CrossRef

Hartmann, D.L. (1994): Global Physical Climatology. Academic Press, 1 ed., 411 pp.

Hoffman, P.F. and Z.X. Li (2009): A palaeogeographic context for Neoproterozoic glaciation. Palaeogeogr. Palaeocl., 277, 158–172.CrossRef

Holton, J.R. (2004): An introduction to dynamic meteorology. Academic Press, 511 pp.

Houghton, J. (2001): The Physics of Atmospheres. Cambridge University Press, 3 ed., 336 pp.

Houghton, J. (2009): Global Warming: The Complete Briefing. Cambridge University Press, 4 ed., 456 pp.

Huber, C., M. Leuenberger, R. Spahni, J. Flückiger, J. Schwander, T.F. Stocker, S. Johnsen, A. Landais, and J. Jouzel (2006): Isotope calibrated Greenland temperature record over Marine Isotope Stage 3 and its relation to CH4. Earth Planet. Sc. Lett., 243, 504–519.CrossRef

IPCC (2001): Climate Change 2001 - The Scientific Basis: Contribution of Working Group I to the Third Assessment Report of the IPCC. Cambridge University Press, 892 pp.

IPCC (2007): Climate Change 2007 - The Physical Science Basis: Working Group I Contribution to the Fourth Assessment Report of the IPCC. Cambridge University Press, 1009 pp.

Jayne, S.R. and J. Marotzke (2002): The oceanic eddy heat transport. J. Phys. Oceanogr., 32, 3328–3345.CrossRef

Joos, F., G.K. Plattner, T.F. Stocker, O. Marchal, and A. Schmittner (1999): Global warming and marine carbon cycle feedbacks on future atmospheric CO2. Science, 284, 464–467.CrossRef

Jouzel, J., V. Masson-Delmotte, O. Cattani, G. Dreyfus, S. Falourd, G. Hoffmann, B. Minster, J. Nouet, J.-M. Barnola, J. Chappellaz, H. Fischer, J.C. Gallet, S. Johnsen, M. Leuenberger, L. Loulergue, D. Lüthi, H. Oerter, F. Parrenin, G. Raisbeck, D. Raynaud, A. Schilt, J. Schwander, E. Selmo, R. Souchez, R. Spahni, B. Stauffer, J.P. Steffensen, B. Stenni, T.F. Stocker, J.L. Tison, M. Werner, and E.W. Wolff (2007): Orbital and millennial Antarctic climate variability over the past 800,000 years. Science, 317, 793–796.CrossRef

Knutti, R. and G.C. Hegerl (2008): The equilibrium sensitivity of the Earths temperature to radiation changes. Nat. Geosci., 1, 735–743.CrossRef

Knutti, R., T.F. Stocker, F. Joos, and G.-K. Plattner (2002): Constraints on radiative forcing and future climate change from observations and climate model ensembles. Nature, 416, 719–723.CrossRef

Knutti, R., T.F. Stocker, F. Joos, and G.K. Plattner (2003): Probabilistic climate change projections using neural networks. Clim. Dyn., 21, 257–272.CrossRef

Knutti, R., J. Flückiger, T.F. Stocker, and A. Timmermann (2004): Strong hemispheric coupling of glacial climate through freshwater discharge and ocean circulation. Nature, 430, 851–856.CrossRef

Kraus, E.B. and J.A. Businger (1994): Atmosphere–Ocean Interaction. Oxford University Press, 362 pp.

Krishnamurti, T.N. and L. Bounoua (1996): An Introduction to Numerical Weather Prediction Techniques. CRC Press, 1 ed., 293 pp.

Lenton, T.M., H. Held, E. Kriegler, J.W. Hall, W. Lucht, S. Rahmstorf, and H.J. Schellnhuber (2008): Tipping elements in the Earth’s climate system. P. Natl. Acad. Sci. USA, 105, 1786–1793.CrossRef

Lorenz, E.N. (1963): Deterministic nonperiodic flow. J. Atmos. Sci., 20, 130–141.CrossRef

Lorenz, E.N. (1979): Forced and free variations of weather and climate. J. Atmos. Sci., 36, 1367–1376.CrossRef

Lorenz, E.N. (1984): Irregularity: A fundamental property of the atmosphere. Tellus, 36, 98–110.

Lorenz, E.N. (1996): The Essence of Chaos. University of Washington Press, 227 pp.

Lozier, M.S. (2010): Deconstructing the conveyor belt. Science, 328, 1507–1511.CrossRef

Lüthi, D., M. Le Floch, B. Bereiter, T. Blunier, J.-M. Barnola, U. Siegenthaler, D. Raynaud, J. Jouzel, H. Fischer, K. Kawamura, and T.F. Stocker (2008): High-resolution carbon dioxide concentration record 650,000–800,000 years before present. Nature, 453, 379–382.CrossRef

Manabe, S. and K. Bryan (1969): Climate calculations with a combined ocean-atmosphere model. J. Atmos. Sci., 26, 786–789.CrossRef

Manabe, S. and R.J. Stouffer (1988): Two stable equilibria of a coupled ocean-atmosphere model. J. Climate, 1, 841–866.CrossRef

Manabe, S. and R.J. Stouffer (1994): Multiple-century response of a coupled ocean-atmosphere model to an increase of atmospheric carbon dioxide. J. Climate, 7, 5–23.CrossRef

Marchal, O., T.F. Stocker, F. Joos, A. Indermühle, T. Blunier, and J. Tschumi (1999): Modelling the concentration of atmospheric CO2 during the Younger Dryas climate event. Clim. Dyn., 15, 341–354.CrossRef

Marotzke, J. (2000): Abrupt climate change and thermohaline circulation: Mechanisms and predictability. P. Natl. Acad. Sci. USA, 97, 1347–1350.CrossRef

McGuffie, K. and A. Henderson-Sellers (2005): A Climate Modelling Primer. Wiley, 3 ed., 296 pp.

Mikolajewicz, U., M. Gröger, E. Maier-Reimer, G. Schurgers, M. Vizcaíno, and A.M.E. Winguth (2007): Long-term effects of anthropogenic CO2 emissions simulated with a complex earth system model. Clim. Dyn., 28, 599–633.CrossRef

Müller, S.A., F. Joos, N.R. Edwards, and T.F. Stocker (2006): Water mass distribution and ventilation time scales in a cost-efficient, three-dimensional ocean model. J. Climate, 19, 5479–5499.CrossRef

Myhre, G., E.J. Highwood, K.P. Shine, and F. Stordal (1998): New estimates of radiative forcing due to well mixed greenhouse gases. Geophys. Res. Lett., 25, 2715–2718.CrossRef

Nakicenovic, N., J. Alcamo, G. Davis, B. de Vries, J. Fenhann, S. Gaffin, K. Gregory, A. Grubler, T.Y. Jung, T. Kram, E.L. La Rovere, L. Michaelis, S. Mori, T. Morita, W. Pepper, H. Pitcher, L. Price, K. Riahi, A. Roehrl, H.-H. Rogner, A. Sankovski, M. Schlesinger, P. Shukla, S. Smith, R. Swart, S. van Rooijen, N. Victor, and Z. Dadi (2000): Special Report on Emissions Scenarios: A Special Report of Working Group III of the Intergovernmental Panel on Climate Change. Cambridge University Press, 598 pp.

North, G.R., D.A. Short, and J.G. Mengel (1983): Simple energy balance model resolving the seasons and the continents - Application to the astronomical theory of the ice ages. J. Geophys. Res., 88, 6576–6586.CrossRef

Oeschger, H., J. Beer, U. Siegenthaler, B. Stauffer, W. Dansgaard, and C.C. Langway (1984): Late glacial climate history from ice cores. In: J. E. Hansen and T. Takahashi (Editors), Climate Processes and Climate Sensitivity, vol. 29 of Geophysical Monograph Series, pp. 299–306. American Geophysical Union.

Pedlosky, J. (1987): Geophysical Fluid Dynamics. Springer, 710 pp.

Peixoto, J.P. and A.H. Oort (1992): Physics of Climate. Springer, 520 pp.

Petit, J.R., J. Jouzel, D. Raynaud, N.I. Barkov, J.-M. Barnola, I. Basile, M. Bender, J. Chappellaz, M. Davis, G. Delaygue, M. Delmotte, V.M. Kotlyakov, M. Legrand, V.Y. Lipenkov, C. Lorius, L. PÉpin, C. Ritz, E. Saltzman, and M. Stievenard (1999): Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature, 399, 429–436.

Phillips, N.A. (1956): The general circulation of the atmosphere: a numerical experiment, QJ Roy. Q. J. Roy. Meteor. Soc., 82, 123–164.CrossRef

Plattner, G.K., R. Knutti, F. Joos, T.F. Stocker, W. von Bloh, V. Brovkin, D. Cameron, E. Driesschaert, S. Dutkiewicz, M. Eby, N.R. Edwards, T. Fichefet, J.C. Hargreaves, C.D. Jones, M.F. Loutre, H.D. Matthews, A. Mouchet, S.A. Müller, S. Nawrath, A. Price, A. Sokolov, K.M. Strassmann, and A.J. Weaver (2008): Long-term climate commitments projected with climate-carbon cycle models. J. Climate, 21, 2721–2751.CrossRef

Press, W.H., B.P. Flannery, S.A. Teukolsky, and W.T. Vetterling (1992): Numerical Recipes in FORTRAN 77: The Art of Scientific Computing, vol. 1. Cambridge University Press, 2 ed., 992 pp.

Press, W.H., S.A. Teukolsky, W.T. Vetterling, and B.P. Flannery (1996): Numerical Recipes in Fortran 90: The Art of Scientific Computing, vol. 2. Cambridge University Press, 2 ed., 500 pp.

Press, W.H., S.A. Teukolsky, W.T. Vetterling, and B.P. Flannery (2007): Numerical Recipes 3rd Edition: The Art of Scientific Computing. Cambridge University Press, 3 ed., 1256 pp.

Rahmstorf, S. (2002): Ocean circulation and climate during the past 120,000 years. Nature, 419, 207–214.CrossRef

Renssen, H., H. Goosse, T. Fichefet, V. Brovkin, E. Driesschaert, and F. Wolk (2005): Simulating the Holocene climate evolution at northern high latitudes using a coupled atmosphere-sea ice-ocean-vegetation model. Clim. Dyn., 24, 23–43.CrossRef

Richardson, L.F. (2007): Weather Prediction by Numerical Process (Cambridge Mathematical Library). Cambridge University Press, 2 ed., 250 pp. Reprint of original 1922.

Ritz, S.P., T.F. Stocker, and S.A. Müller (2008): Modeling the effect of abrupt ocean circulation change on marine reservoir age. Earth Planet. Sc. Lett., 268, 202–211.CrossRef

Ritz, S.P., T.F. Stocker, and F. Joos (2011): A coupled dynamical ocean-energy balance atmosphere model for paleoclimate studies. J. Climate, 24, 349–375.CrossRef

Robock, A. (2008): 20 reasons why geoengineering may be a bad idea. Bull. At. Sci., 64, 14–18.CrossRef

Robock, A., L. Oman, and G.L. Stenchikov (2008): Regional climate responses to geoengineering with tropical and Arctic SO₂ injections. J. Geophys. Res., 113, D16101.CrossRef

Ruddiman, W.F. (2007): Earth’s Climate: Past and Future. W.H. Freeman, 2 ed., 388 pp.

Saha, S., S. Nadiga, C. Thiaw, J. Wang, W. Wang, Q. Zhang, H. M. Van den Dool, H.-L. Pan, S. Moorthi, D. Behringer, D. Stokes, M. Peña, S. Lord, G. White, W. Ebisuzaki, P. Peng, and P. Xie (2006): The NCEP climate forecast system. J. Climate, 19, 3483–3517.CrossRef

Saltzman, B. (1962): Finite amplitude free convection as an initial value problem: I. J. Atmos. Sci., 19, 329–341.CrossRef

Saltzman, B. (2001): Dynamical Paleoclimatology: Generalized Theory of Global Climate Change. Academic Press, 354 pp.

Sausen, R., K. Barthel, and K. Hasselmann (1988): Coupled ocean-atmosphere models with flux correction. Clim. Dyn., 2, 145–163.CrossRef

Schär, C., P.L. Vidale, D. Lüthi, C. Frei, C. Häberli, M.A. Liniger, and C. Appenzeller (2004): The role of increasing temperature variability in European summer heatwaves. Nature, 427, 332–336.CrossRef

Schiller, A., U. Mikolajewicz, and R. Voss (1997): The stability of the North Atlantic thermohaline circulation in a coupled ocean-atmosphere general circulation model. Clim. Dyn., 13, 325–347.CrossRef

Schwarz, H.R. (2004): Numerische Mathematik. Teubner B.G. GmbH, 573 pp.CrossRef

Sellers, W.D. (1969): A global climatic model based on the energy balance of the earth-atmosphere system. J. Appl. Meteorol., 8, 392–400.CrossRef

Siedler, G., J. Church, and J. Gould (Editors) (2001): Ocean Circulation and Climate: Observing and Modeling the Global Ocean, vol. 77 of International Geophysics Series. Academic Press, 715 pp.

Siegenthaler, U. and F. Joos (1992): Use of a simple model for studying oceanic tracer distributions and the global carbon cycle. Tellus B, 44, 186–207.CrossRef

Siegenthaler, U., T.F. Stocker, E. Monnin, D. Lüthi, J. Schwander, B. Stauffer, D. Raynaud, J.-M. Barnola, H. Fischer, V. Masson-Delmotte, and J. Jouzel (2005): Stable carbon cycle-climate relationship during the late Pleistocene. Science, 310, 1313–1317.CrossRef

Smolarkiewicz, P.K. (1983): A simple positive definite advection scheme with small implicit diffusion. Mon. Weather Rev., 111, 479–486.CrossRef

Soden, B.J. and I.M. Held (2006): An assessment of climate feedbacks in coupled ocean–atmosphere models. J. Climate, 19, 3354–3360.CrossRef

Soden, B.J., R.T. Wetherald, G.L. Stenchikov, and A. Robock (2002): Global cooling after the eruption of Mount Pinatubo: A test of climate feedback by water vapor. Science, 296, 727–730.CrossRef

Stocker, T.F. (1998): The seesaw effect. Science, 282, 61–62.CrossRef

Stocker, T.F. (2000): Past and future reorganizations in the climate system. Quaternary Sci. Rev., 19, 301–319.CrossRef

Stocker, T.F. (2003): South dials north. Nature, 424, 496–499.CrossRef

Stocker, T.F. and S.J. Johnsen (2003): A minimum thermodynamic model for the bipolar seesaw. Paleoceanography, 18, 1087.CrossRef

Stocker, T.F. and O. Marchal (2000): Abrupt climate change in the computer: Is it real? P. Natl. Acad. Sci. USA, 97, 1362–1365.CrossRef

Stocker, T.F. and A. Schmittner (1997): Influence of CO2 emission rates on the stability of the thermohaline circulation. Nature, 388, 862–865.CrossRef

Stocker, T.F. and D.G. Wright (1991): A zonally averaged ocean model for the thermohaline circulation. Part II: Interocean circulation in the Pacific-Atlantic basin system. J. Phys. Oceanogr., 21, 1725–1739.

Stocker, T.F., D.G. Wright, and L.A. Mysak (1992): A zonally averaged, coupled ocean-atmosphere model for paleoclimate studies. J. Climate, 5, 773–797.CrossRef

Stommel, H. (1948): The westward intensification of wind-driven ocean currents. Trans. Amer. Geophys. Union, 29, 202–206.CrossRef

Stommel, H. (1958): The abyssal circulation. Deep Sea Res., 5, 80–82.CrossRef

Stommel, H. (1961): Thermohaline convection with two stable regimes of flow. Tellus, 13, 224–230.CrossRef

Stommel, H. and A.B. Arons (1960): On the abyssal circulation of the world ocean–I. Stationary planetary flow patterns on a sphere. Deep Sea Res., 6, 140–154.

Stroeve, J., M.M. Holland, W. Meier, T. Scambos, and M. Serreze (2007): Arctic sea ice decline: Faster than forecast. Geophys. Res. Lett., 34, L09501.CrossRef

Trenberth, K.E. (Editor) (1992): Climate System Modeling. Cambridge University Press, 1 ed., 818 pp.

Trenberth, K.E., J.M. Caron, and D.P. Stepaniak (2001): The atmospheric energy budget and implications for surface fluxes and ocean heat transports. Clim. Dyn., 17, 259–276.CrossRef

Trenberth, K.E., J.T. Fasullo, and J. Kiehl (2009): Earth’s global energy budget. B. Am. Meteorol. Soc., 90, 311–323.CrossRef

UNFCCC (1992): United Nations Framework Convention on Climate Change. United Nations. URL http://unfccc.int.

Uppala, S.M., P.W. Kållberg, A.J. Simmons, U. Andrae, V.D.C. Bechtold, M. Fiorino, J.K. Gibson, J. Haseler, A. Hernandez, G.A. Kelly, X. Li, K. Onogi, S. Saarinen, N. Sokka, R.P. Allan, E. Andersson, K. Arpe, M.A. Balmaseda, A.C.M. Beljaars, L. Van De Berg, J. Bidlot, N. Bormann, S. Caires, F. Chevallier, A. Dethof, M. Dragosavac, M. Fisher, M. Fuentes, S. Hagemann, E. Hólm, B.J. Hoskins, L. Isaksen, P.A.E.M. Janssen, R. Jenne, A.P. Mcnally, J.-F. Mahfouf, J.-J. Morcrette, N.A. Rayner, R.W. Saunders, P. Simon, A. Sterl, K.E. Trenberth, A. Untch, D. Vasiljevic, P. Viterbo, and J. Woollen (2005): The ERA-40 re-analysis. Q. J. Roy. Meteor. Soc., 131, 2961–3012.CrossRef

Velicogna, I. (2009): Increasing rates of ice mass loss from the Greenland and Antarctic ice sheets revealed by GRACE. Geophys. Res. Lett., 36, L19503.CrossRef

Washington, W.M. and C.L. Parkinson (2005): Introduction to Three-dimensional Climate Modeling. University Science Books, 2 ed., 368 pp.

Wild, M. (2000): Absorption of solar energy in cloudless and cloudy atmospheres over Germany and in GCMs. Geophys. Res. Lett., 27, 959–962.CrossRef

Willebrand, J. (1993): Forcing the ocean by heat and freshwater fluxes. In: E. Raschke and D. Jacob (Editors), Energy and Water Cycles in the Climate System, pp. 215–233. Springer.

Winton, M. (2006): Surface albedo feedback estimates for the AR4 climate models. J. Climate, 19, 359–365.CrossRef

Woodruff, S.D., R.J. Slutz, R.L. Jenne, and P.M. Steurer (1987): A Comprehensive Ocean-Atmosphere Data Set. B. Am. Meteorol. Soc., 68, 1239–1250.CrossRef

Zaucker, F., T.F. Stocker, and W.S. Broecker (1994): Atmospheric freshwater fluxes and their effect on the global thermohaline circulation. J. Geophys. Res., 99, 12443–12457.CrossRef

Titel: Atmosphere–Ocean Interactions
verfasst von: Thomas Stocker
Verlag: Springer Berlin Heidelberg
Buch: Introduction to Climate Modelling
Print ISBN: 978-3-642-00772-9

Electronic ISBN: 978-3-642-00773-6

Copyright-Jahr: 2011
DOI: https://doi.org/10.1007/978-3-642-00773-6_8