331
MILANKOVIC, M., 1930: Mathematische Klimalehre und astronomische Theorie der Klimaschwankungen, Handbuch der Klimatologie, BdI, Teil A, Hrg. Koppen/Geiger, Berlin,
1930.
MILLER, M. J., T. N. PALMER AND R. SWINBANK, 1989: Parameterization and influence of
sub-grid scale orography in general circulation and numerical weather prediction models.
Met. Atm. Phys., 40, 84-109.
MITCHELL, J. F. B., T.C. JOHNS, J. M. GREGORY AND S. TETT, 1995: Transient climate
response to increasing sulfate aerosols and greenhouse gases. Nature, 376, 501-504.
MOLLER, F., 1963: On the influence of changes in C02 concentration in air on the radiative
balance of the earth's surface and on the climate. J. Geophys. Res., 68, 3877-3886.
MURPHY, J. M., 1990: Prediction of the transient response of climate to a gradual increase
in C02, using a coupled ocean/atmospheric model with flux correction. In: Research
Activities in Atmospheric and Ocean Modelling. CAS/JSC Working Group on Numerical
Experimentation, Report No. 14, WMO/TD No 396, 9.7-9.8.
MURPHY, J. M. AND J. F. B. MITCHELL, 1995: Transient response of the Hadley Centre
coupled model to increasing carbon dioxide. Part II - Temporal and spatial evolution of
patterns. J. Climate, 8, 57-80.
NEELIN, J.D., M. LATIF, M.A.F. ALLAART, M. CANE, U. CUBASCH, W.L. GATES, P.R.
GENT, M. GHIL, C. GORDON, N.C. LAU, N.C. MECHOSO, G.A. MEEHL, J.M. OBERHUBER, S.G.H. PHILANDER, P.S. SCHOPF, K.R. SPERBER, A. STERL, T. TOKIOKA,
J. TRIBBIA AND S.E. ZEBIAK, 1992: Tropical air-sea interaction in general circulation
models. Clim. Dyn., 7, 73-104.
NEFTEL, A., J. BEER, H. OESCHGER, F. ZURCHER AND R. C. FINKEL, 1985: Sulphate and
nitrate concentrations in snow from South Greenland 1895-1978. Nature, 314, 611-613.
NORDENG, T., 1994: Extended versions of the convective parameterization scheme at ECMWF
and their impact on the mean and transient activity of the model in the tropics.ECMWF,
Research Department, Technical Memorandum No.206, October 1994, 41pp., submitted
to Q. J. R. Meteorol. Soc.
OBERHUBER, J.M., 1988: An atlas based on the 'COADS' data set: The budgets of heat,
buoyancy and turbulent kinetic energy at the surface of the global ocean. Max-PlanckInstitut fiir Meteorologie, Report No. 15, Hamburg.
OBERHUBER, J .M., 1993A: Simulation of the Atlantic circulation with a coupled sea ice-mixed
layer-isopycnal general circulation model. Part I: Model description. J. Phys. Oceanogr.,
22, 808-829.
OBERHUBER, J.M., 1993B: The OPYC Ocean General Circulation Model. Deutsches Klimarechenzentrum GmbH, Technical Report No.7, Hamburg.
o HMURA , A. AND H. GILGEN, 1993: Re-evaluation of the global energy balance. Geophysical
Monograph 75, IUGG Volume 5, 93-110.
PALMER, T.N., G. J. SHUTTS AND R. SWINBANK, 1986: Alleviationofa systematic westerly
bias in general circulation and numerical weather prediction models through an orographic
gravity wave drag parameterization. Quart. J. Roy. Meteor. Soc., 112, 1001-1031.
MILANKOVIC, M., 1930: Mathematische Klimalehre und astronomische Theorie der Klimaschwankungen, Handbuch der Klimatologie, BdI, Teil A, Hrg. Koppen/Geiger, Berlin,
1930.
MILLER, M. J., T. N. PALMER AND R. SWINBANK, 1989: Parameterization and influence of
sub-grid scale orography in general circulation and numerical weather prediction models.
Met. Atm. Phys., 40, 84-109.
MITCHELL, J. F. B., T.C. JOHNS, J. M. GREGORY AND S. TETT, 1995: Transient climate
response to increasing sulfate aerosols and greenhouse gases. Nature, 376, 501-504.
MOLLER, F., 1963: On the influence of changes in C02 concentration in air on the radiative
balance of the earth's surface and on the climate. J. Geophys. Res., 68, 3877-3886.
MURPHY, J. M., 1990: Prediction of the transient response of climate to a gradual increase
in C02, using a coupled ocean/atmospheric model with flux correction. In: Research
Activities in Atmospheric and Ocean Modelling. CAS/JSC Working Group on Numerical
Experimentation, Report No. 14, WMO/TD No 396, 9.7-9.8.
MURPHY, J. M. AND J. F. B. MITCHELL, 1995: Transient response of the Hadley Centre
coupled model to increasing carbon dioxide. Part II - Temporal and spatial evolution of
patterns. J. Climate, 8, 57-80.
NEELIN, J.D., M. LATIF, M.A.F. ALLAART, M. CANE, U. CUBASCH, W.L. GATES, P.R.
GENT, M. GHIL, C. GORDON, N.C. LAU, N.C. MECHOSO, G.A. MEEHL, J.M. OBERHUBER, S.G.H. PHILANDER, P.S. SCHOPF, K.R. SPERBER, A. STERL, T. TOKIOKA,
J. TRIBBIA AND S.E. ZEBIAK, 1992: Tropical air-sea interaction in general circulation
models. Clim. Dyn., 7, 73-104.
NEFTEL, A., J. BEER, H. OESCHGER, F. ZURCHER AND R. C. FINKEL, 1985: Sulphate and
nitrate concentrations in snow from South Greenland 1895-1978. Nature, 314, 611-613.
NORDENG, T., 1994: Extended versions of the convective parameterization scheme at ECMWF
and their impact on the mean and transient activity of the model in the tropics.ECMWF,
Research Department, Technical Memorandum No.206, October 1994, 41pp., submitted
to Q. J. R. Meteorol. Soc.
OBERHUBER, J.M., 1988: An atlas based on the 'COADS' data set: The budgets of heat,
buoyancy and turbulent kinetic energy at the surface of the global ocean. Max-PlanckInstitut fiir Meteorologie, Report No. 15, Hamburg.
OBERHUBER, J .M., 1993A: Simulation of the Atlantic circulation with a coupled sea ice-mixed
layer-isopycnal general circulation model. Part I: Model description. J. Phys. Oceanogr.,
22, 808-829.
OBERHUBER, J.M., 1993B: The OPYC Ocean General Circulation Model. Deutsches Klimarechenzentrum GmbH, Technical Report No.7, Hamburg.
o HMURA , A. AND H. GILGEN, 1993: Re-evaluation of the global energy balance. Geophysical
Monograph 75, IUGG Volume 5, 93-110.
PALMER, T.N., G. J. SHUTTS AND R. SWINBANK, 1986: Alleviationofa systematic westerly
bias in general circulation and numerical weather prediction models through an orographic
gravity wave drag parameterization. Quart. J. Roy. Meteor. Soc., 112, 1001-1031.