Sentences with phrase «middle atmosphere model»

Rind, D., R. Suozzo, and N.K. Balachandran, 1988: The GISS Global Climate - Middle Atmosphere Model.

Changes in tracer distribution in the troposphere and stratosphere are calculated from a control and doubled CO2 climate simulation run with the Goddard Institute for Space Studies Global Climate Middle Atmosphere Model.

Langematz, U., J.L Grenfell, K. Matthes, and M. Kunze, 2004: Chemical effects in 11 - year solar cycle simulations with the Freie Universitaet Berlin Climate Middle Atmosphere Model (FUB - CMAM - CHEM), Geophys.

Beagley, S.R., J. de Grandpré, J.N. Koshyk, N.A. McFarlane, and T.G. Shepherd, 1997: Radiative - dynamical climatology of the first - generation Canadian Middle Atmosphere Model.

de Grandpré, J., S.R. Beagley, V.I. Fomichev, E. Griffioen, J.C. McConnell, A.S. Medvedev, and T.G. Shepherd, 2000: Ozone climatology using interactive chemistry: Results from the Canadian Middle Atmosphere Model, J. Geophys.

Not exact matches

1: Present day climatology and interannual variability of the middle atmosphere using the model and 9 years of HALOE / UARS data, J. Geophys.

1990 bis 1995 Mitglied der Arbeitsgruppe 5 des «Solar - Terrestrial Energy Program» (STEP); Leiter der Aktivität 5.3 «Modelling of possible solar variability effects in the lower and middle atmosphere» (MELA)

``... it is concluded that comprehensive climate model studies require a middle atmosphere as well as a coupled ocean to investigate and understand natural climate variability.»

-- First we increase the greenhouse gases — then that causes warming in the atmosphere and oceans — as the oceans warm up, they evaporate more H2O — more moisture in the air means more precipitation (rain, snow)-- the southern hemisphere is essentially lots of water and a really big ice cube in the middle called Antarctica — land ice is different than sea ice — climate models indicated that more snowfall would cause increases in the frozen H2O — climate models indicated that there would be initial increases in sea ice extent — observations confirm the indications and expectations that precipitation is increasing, calving rates are accelerating and sea ice extent is increasing.