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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创新

Radiative Forcing by Tropospheric Ozone Changes due to Increased Emissions of CH4, CO and NOxor (CH., CO, NO.) emissions and to calculate the associated radiative forcing on the climate system. Significant perturbations of tropospheric ozone photochemical produetion and consequently of ozone concentrations are calculated, with important seasonal and latitudinal dependences. For all simulati

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The Role of Convection in the Vertical Distribution of Ozone and Precursors in the Troposphereconnection with convective clouds and frontal circulation is about 0.6 TgN/yr, and in addition about the same amount of other NO. compounds is injected. For comparison, the various sources at the ground total 34 TgN/yr of NO.. The strength of the lightning source was assumed to be 3 TgN/yr. The tota

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incisive

Ozone Chemistry Changes in the Troposphere and Consequent Radiative Forcing of Climatephere since pre-industrial times. Calculated increases of tropospheric O. have been evaluated with a radiative transfer model. Our calculations confirm earlier studies that the combined effects of anthropogenic NO., CO and CH. emissions cause a strong enhancement of O. levels throughout the global t

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A GCM Study of the Climatic Effect of 1979–1992 Ozone TrendM). The GCM employs a newly constructed ozone climatology that includes longitudinal Variation. In the perturbed Simulation, the O. trend is assumed to be confined to the lower stratosphere, and imposed in transient from January 1979 to December 1992 to incorporate both seasonal variations and linea

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Sätze von Bloch, Picard und Schottkyer stratospheric ozone. There has been statistically significant increases in free tropospheric ozone concentration in some areas of the northem hemisphere and, at the same time, a global decrease in lower stratospheric ozone concentration. The total ozone continues to decline by an average rate of

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陈旧

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Unendliche Produkte holomorpher Funktionentraviolet radiation and outgoing infrared radiation. It also indirectly affects climate because it is intimately linked with the concentration of OH in the troposphere, which ultimately determines the fate of many trace gases (including greenhouse gases). In this paper, we illustrate how climate-rel