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Titlebook: Chemistry and Radiation Changes in the Ozone Layer; Christos S. Zerefos (Professor, Director),Ivar S. Book 2000 Springer Science+Business

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发表于 2025-3-21 19:04:49 | 显示全部楼层 |阅读模式
书目名称Chemistry and Radiation Changes in the Ozone Layer
编辑Christos S. Zerefos (Professor, Director),Ivar S.
视频videohttp://file.papertrans.cn/225/224806/224806.mp4
丛书名称Nato Science Series C:
图书封面Titlebook: Chemistry and Radiation Changes in the Ozone Layer;  Christos S. Zerefos (Professor, Director),Ivar S.  Book 2000 Springer Science+Business
描述Recent studies have demonstrated a link between ozone changescaused by human activities and changing UV levels at the Earth‘ssurface, as well as a link to climate through changes in radiativeforcing and links to changes in chemical composition. .This book draws together key scientists who provide state of the artcontributions on the variable ozone layer and the interplay oflongwave and shortwave radiative interactions which link ozone, theclimate and UV issues.
出版日期Book 2000
关键词Aerosol; Ozone layer; Radiometer; Troposphere; atmosphere; experiment; sferic; spheric; theory
版次1
doihttps://doi.org/10.1007/978-94-011-4353-0
isbn_softcover978-0-7923-6514-3
isbn_ebook978-94-011-4353-0Series ISSN 1389-2185
issn_series 1389-2185
copyrightSpringer Science+Business Media Dordrecht 2000
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Model Analysis of Stratosphere-Troposphere Exchange of Ozone and Its Role in the Tropospheric Ozoneconsiderably during industrialization as a result of the photochemical transformation of anthropogenically emitted ozone precursors such as nitrogen oxides (NO.), methane (CH.), carbon monoxide (CO), and nonmethane hydrocarbons (NMHC) [1]. Analysis of measurement data from the second half of the las
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Global Impact of Aircraft Emission on Ozone Concentrations and Methane Lifetime: Results from the 1 IPCCassessment of aircraft emissions. 6 modelling groups participated, and extensive model studies with global scale CTMs, and one GCM were performed. The main emphasis in the study was on estimates of future (2015 and 2050) perturbations. Studies were also performed where sensitivities to model fo
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Tropospheric Aerosol Formation: Processes, Observations and Simulations,il dust, sea salt spray, smoke and ash), and dispersed sources due to gas-to-particle conversion. New simultaneous measurements of ultrafine particles (i.e., having sizes from ~3–20 nm) and precursor vapor concentrations (notably H.SO.) [3–8] provides new windows into understanding natural aerosol f
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