Titlebook: Atmospheric Ozone as a Climate Gas; General Circulation Wei-Chyung Wang,Ivar S. A. Isaksen Conference proceedings 1995 Springer-Verlag Ber

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Upper Tropospheric/Lower Stratospheric Ozone Climatologyion in Australia and one in Brazil, however with periods with a measurement frequency less than one sonde per week. In general, the data quality is uneven between these stations. If a better assessment is to be made of ozone impaets on climate, research must establish the trend in ozone concentratio

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Simulations of Stratospheric Ozone in a Climate Modelhe 42 level model. In contrast, the 19 level model had not produced a warming by the end of the integration on 22 March, but predicted a further cold spell in early March together with additional PSCs and ozone destruction. Since final warmings in the Arctic nearly always occur before this date, it

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Concurrent Ozone and Temperature Trends Derived from Ozonesonde Stationsly significant surface warming over the past two decades. Above the South Pole, an observed strong cooling during November month can be simulated with a radiative transfer model under the concept of fixed dynamical heating, due to the observed ozone hole deepening one month earlier.

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Ozone Chemistry Changes in the Troposphere and Consequent Radiative Forcing of Climate27 Tg/yr, caused mostly by anthropogenic emissions in the mid- latitude northern hemisphere and to a lesser extent by biomass burning emissions in the tropics. We calculate that the global O. burden in the troposphere has increased by a factor of 1.7, the CO burden by a factor of 2.5 and that of H.O

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A GCM Study of the Climatic Effect of 1979–1992 Ozone Trende forcing expectations. Over the Arctic, a relatively small O. loss leads the model stratosphere to warm substantially during November-January. This is followed by a strong cooling in March-May. The result cannot be attributed exclusively to the radiative forcing. Rather it indicates the dominant ro

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Unendliche Produkte holomorpher Funktionenions. However, the effect may be compensated for if cloudiness increases. A temperature increase of 4.2° C produced a global increase of 30% in lightning activity (70% over continental regions), which will increase both NO. and O. aloft. Finally, changes in convective activity may either increase or