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Atmospheric Ozone As a Climate Gas General Circulation Model Simulations (Nato a S I Series Series I, Global Environmental Change) by

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Published by Springer-Verlag Telos .
Written in English


  • Atmospheric regions,
  • Chemical spectroscopy, spectrochemistry,
  • Weather,
  • Environmental aspects,
  • Congresses,
  • Science,
  • Science/Mathematics,
  • Greenhouse gases,
  • Earth Sciences - Meteorology & Climatology,
  • Atmospheric ozone,
  • Earth Sciences - General,
  • Atmospheric Chemistry,
  • Mathematical Models

Book details:

Edition Notes

ContributionsWei-Chyung Wang (Editor), I. S. A. Isaksen (Editor)
The Physical Object
Number of Pages459
ID Numbers
Open LibraryOL9061557M
ISBN 103540600094
ISBN 109783540600091

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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 , a NATO workshop on atmospheric ozone was held in Lillehammer. Atmospheric Impacts of the Oil and Gas Industry provides the most up-to-date scientific and technological methods available to quantify oil and gas industry emissions and atmospheric impacts in a manner that is relevant to the development of, compliance with, and enforcement of effective policy and regulations. The book offers a concise survey. Wei-Chyung Wang, Kendal McGuffie, in The Future of the World's Climate (Second Edition), The Role of Ozone As a Climatically Active Compound. Atmospheric ozone has been recognized as a climatically active gas (Wang and Isaksen, ) and its change will affect atmospheric temperature, as well as the solar and longwave radiation reaching the surface. The atmospheric pressure at the top of the stratosphere is roughly 1/ the pressure at sea level. It contains the ozone layer, which is the part of Earth's atmosphere that contains relatively high concentrations of that gas. The stratosphere defines a layer in .

ISBN: OCLC Number: Notes: "Proceedings of the Advanced Study Institute on Atmospheric Ozone as a Climate Gas, held in Lillehammer, Norway, June , "--Title page verso. The lecture addresses “atmospheric ozone as a climate gas” with a broader perspective, covering the greenhouse effect, the radiative and chemical processes of atmospheric O 3, the concept of radiative forcing for climate change, and then the case studies of aircraft emissions involving O : Wei-Chyung Wang, Ivar S. A. Isaksen, Jing Wang, Michael Gauss, Xin-Zhong Liang, Xin-Zhong Liang. Get this from a library! Atmospheric ozone as a climate gas: general circulation model simulations. [Wei-Chyung Wang; I S A Isaksen; North Atlantic Treaty Organization. Scientific Affairs Division,;] -- This book treats in detail the physical, chemical, and dynamic processes that influence atmospheric ozone in the lower stratosphere and upper troposphere. Chapter 4 of the IPCC Third Assessment Report Climate Change The Scientific Basis. Sections include: Executive Summary Introduction Trace Gases: Current Observations, Trends and Budgets Projections of Future Emissions Projections of .

OZONE-DEPLETION-GREENHOUSE-GASES-AND-CLIMATE-CHANGE Download Ozone-depletion-greenhouse-gases-and-climate-change ebook PDF or Read Online books in PDF, EPUB, and Mobi Format. Click Download or Read Online button to OZONE-DEPLETION-GREENHOUSE-GASES-AND-CLIMATE-CHANGE book pdf for free now. Atmospheric ozone is present in very small amounts in the lower atmosphere. However, it begins to increase in abundance at about km elevation, marking the base of the stratosphere. Ozone reaches a maximum at around 25 km, which constitutes the center of the well-known ozone layer. Ozone (O 3) is a trace gas of the troposphere, with an average concentration of 20–30 parts per billion by volume (ppbv), with close to ppbv in polluted areas. Ozone is also an important constituent of the stratosphere, where the ozone layer exists which is located between 10 and 50 kilometers about the earths surface. The troposphere is the lowest layer of the Earth's atmosphere. First, a modern trend of increas- ing global atmospheric CH4 has been documented in the trapped gas in polar ice cores (Craig and Chou, ; Khali! and Rasmussen, ) and with regular monitoring of ambient CH4 at remote lo- cations around the world (Steele et al., ; Blake and Rowland, ~.