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Inhaltsangabe
This book investigates elementary processes in the Earth’s atmosphere involving photons, electrons, ions, radicals, and aerosols. It is based on global atmospheric models such as the standard atmospheric model with averaged atmospheric parameters across the globe and over time, the Earth’s energetic balance, and the global electric circuit that allows to analyze fundamental atmospheric properties to be analyzed. Rate constants of elementary processes in the Earth’s atmosphere, together with measured atmospheric parameters and existing concepts of atmospheric phenomena, are used in the analysis of global and local atmospheric processes. Atmospheric photoprocesses result from the interaction of solar radiation with the atmosphere and processes involving ions, oxygen atoms, excited atomic particles and ozone molecules. Atmospheric electricity as a secondary phenomenon to atmospheric water circulation results in a chain of processes that begins with collisions of water aerosols in different aggregate states. Cosmic rays are of importance for atmospheric electricity, as they create positive and negative ions in the air. Air breakdown in an electric field of clouds in the form of lightning may develop under the influence of cosmic ray-created seed electrons, which are necessary for electron multiplication in ionization wave-streamers. The upper atmosphere (ionosphere) is formed under solar radiation in a vacuum ultraviolet spectrum, and absorption of this radiation leads to air photoionization. The greenhouse effect is determined by atmospheric water, whereas transitions between a water vapor and aerosols may lead to a change in atmospheric optical depth. Carbon dioxide contributes in small portions to the atmospheric greenhouse effect. Cosmic rays are of importance for atmospheric discharge, the origin of lightning and cloud formation in the first stage ofaerosol growth. This book provides a qualitative description of atmospheric properties and phenomena based on elementary processes and simple models.
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Über die Autorin bzw. den Autor
Boris Smirnov was born in 1938 in Moscow. In 1962 he graduated from Moscow's Engineering-Physical Institute in Theoretical Nuclear Physics. He got the dissertation of Candidate of Phys. Mat. Science in 1964, and Doctor of Phys. Mat. Science in 1968. He became a Professor of Physics in 1970. In the years 1962-1982 he was Head of Laboratory at Kurchatov Institute of Atomic Energy (Moscow), from 1982-1986 Head of Laboratory at Institute of Thermophysics (Novosibirsk) and from 1986 Head of Laboratory, Head of Department and now Principal Scientific at Joint Institute for High Temperatures of Russian Academy of Science. B.M. Smirnov was a member of the editorial Board of several journals of various publishers. He was Professor of the Moscow Power Institute, Novosibirsk, State University and the Moscow Institute of Science and Technology. He was a laureate of the National Prize of Russia. His research is focused on Theoretical Physics, Atomic, Molecular, Cluster, Plasma and ChemicalPhysics. He is author of 53 books and about 500 papers.
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This book investigates elementary processes in the Earth’s atmosphere involving photons, electrons, ions, radicals, and aerosols. It is based on global atmospheric models such as the standard atmospheric model with averaged atmospheric parameters across the globe and over time, the Earth’s energetic balance, and the global electric circuit that allows to analyze fundamental atmospheric properties to be analyzed. Rate constants of elementary processes in the Earth’s atmosphere, together with measured atmospheric parameters and existing concepts of atmospheric phenomena, are used in the analysis of global and local atmospheric processes. Atmospheric photoprocesses result from the interaction of solar radiation with the atmosphere and processes involving ions, oxygen atoms, excited atomic particles and ozone molecules. Atmospheric electricity as a secondary phenomenon to atmospheric water circulation results in a chain of processes that begins with collisions of water aerosols in different aggregate states. Cosmic rays are of importance for atmospheric electricity, as they create positive and negative ions in the air. Air breakdown in an electric field of clouds in the form of lightning may develop under the influence of cosmic ray-created seed electrons, which are necessary for electron multiplication in ionization wave-streamers. The upper atmosphere (ionosphere) is formed under solar radiation in a vacuum ultraviolet spectrum, and absorption of this radiation leads to air photoionization. The greenhouse effect is determined by atmospheric water, whereas transitions between a water vapor and aerosols may lead to a change in atmospheric optical depth. Carbon dioxide contributes in small portions to the atmospheric greenhouse effect. Cosmic rays are of importance for atmospheric discharge, the origin of lightning and cloud formation in the first stage of aerosol growth. This book provides a qualitative description of atmospheric properties and phenomena based on elementary processes and simple models.
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- VerlagSpringer
- Erscheinungsdatum2016
- ISBN 10 3319308122
- ISBN 13 9783319308128
- EinbandTapa dura
- SpracheEnglisch
- Auflage1
- Anzahl der Seiten282
- Kontakt zum HerstellerNicht verfügbar
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Microphysics of Atmospheric Phenomena.
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ISBN 10: 3319308122
ISBN 13: 9783319308128
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Microphysics of Atmospheric Phenomena
Verlag:
Springer International Publishing, 2016
ISBN 10: 3319308122
ISBN 13: 9783319308128
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Buch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - This book investigates elementary processes in the Earth's atmosphere involving photons,electrons, ions, radicals, and aerosols. It is based on global atmospheric models such as thestandard atmospheric model with averaged atmospheric parameters across the globe andover time, the Earth's energetic balance, and the global electric circuit that allows to analyzefundamental atmospheric properties to be analyzed. Rate constants of elementary processesin the Earth's atmosphere, together with measured atmospheric parameters and existingconcepts of atmospheric phenomena, are used in the analysis of global and local atmosphericprocesses. Atmospheric photoprocesses result from the interaction of solar radiation withthe atmosphere and processes involving ions, oxygen atoms, excited atomic particles andozone molecules. Atmospheric electricity as a secondary phenomenon to atmospheric watercirculation results in a chain of processes that begins with collisions of water aerosols indifferent aggregate states. Cosmic rays are of importance for atmospheric electricity, asthey create positive and negative ions in the air. Air breakdown in an electric field ofclouds in the form of lightning may develop under the influence of cosmic ray-created seedelectrons, which are necessary for electron multiplication in ionization wave-streamers. Theupper atmosphere (ionosphere) is formed under solar radiation in a vacuum ultravioletspectrum, and absorption of this radiation leads to air photoionization. The greenhouseeffect is determined by atmospheric water, whereas transitions between a water vapor andaerosols may lead to a change in atmospheric optical depth. Carbon dioxide contributesin small portions to the atmospheric greenhouse effect. Cosmic rays are of importancefor atmospheric discharge, the origin of lightning and cloud formation in the first stageofaerosol growth. This book provides a qualitative description of atmospheric propertiesand phenomena based on elementary processes and simple models. Artikel-Nr. 9783319308128
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Microphysics of Atmospheric Phenomena (Springer Atmospheric Sciences)
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