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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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發(fā)表于 2025-3-21 18:40:50 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
期刊全稱Atmospheric Ozone as a Climate Gas
期刊簡稱General Circulation
影響因子2023Wei-Chyung Wang,Ivar S. A. Isaksen
視頻videohttp://file.papertrans.cn/165/164634/164634.mp4
學(xué)科分類Nato ASI Subseries I:
圖書封面Titlebook: Atmospheric Ozone as a Climate Gas; General Circulation  Wei-Chyung Wang,Ivar S. A. Isaksen Conference proceedings 1995 Springer-Verlag Ber
影響因子One of the major findings in the 1992 IPCC report and the 1994 World Meteorological Organization‘s Ozone Assessment report was the identification of possible climatic effects over the last few decades resulting from anthropogenic ally-induced changes in atmospheric ozone. The initial quantitative estimates of their direct climatic effects indicate significant impacts, though large uncertainties exist and studies using general circulation models are needed. A point that needs to be addressed in particular is that atmospheric ozone differs from greenhouse gases in that it is formed and destroyed by chemical processes in the atmosphere due to interaction involving a large number of source gases (e. g. H0, NO ‘ CO, 2 x NMHC, N0, CH and the CFCs). Therefore, the indirect effect of climate-chemistry 2 4 interaction involving atmospheric ozone is an important aspect for consideration in general circulation models. During the last few years, there have been several international workshops related to atmospheric ozone. In 1987, a NATO workshop on atmospheric ozone was held in Lillehammer, Norway. More recently, two workshops were organized to discuss the topic "General Circulation Model Stu
Pindex Conference proceedings 1995
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Climate Modelingtool that can give a first estimate of the possible importance of those changes, while a more detailed understanding may be obtained from experiments using general circulation models (GCMs). These models can be used for sensitivity studies of the climatic response to prescribed ozone changes, howeve
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Issues Relevant to the Development of Coupled Chemistry/Climate Modelsur decades. In the past, this belief has led to the development of two separate efforts: to understand and build models to describing the physical climate system and to understand and build models of the chemical climate system. But how will these two systems interact? Are there important chemical c
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Analysis of 25 years of regular ozone soundings at Uccle (Belgium)und statistically significant trends in tropospheric ozone are found that vary between approximately 1.6% near the surface and 1% per year above the mixed layer. Year-round negative ozone trends are found above 18 km and at the level of the secondary ozone maximum in the lower stratosphere during la
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Concurrent Ozone and Temperature Trends Derived from Ozonesonde Stationsonde stations, 11 of which are in the Northern Hemisphere. The regression analysis takes into account the seasonal, solar and quasi biennial cycles, plus events like volcanic eruptions and instrument change. For all stations, a significant negative ozone trend in (some regions of) the stratosphere i
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