feigelson e m (13 Ergebnisse)

Zustand: Good. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. In good all round condition. No dust jacket. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,650grams, ISBN:

Zustand: Very Good. First edition copy. . 1st U.S. edition. Transactions (Trudy) of the Institute of Atmospheric Physics No. 1. Owner's name on front endpage. This book presents a theoretical and computational study of the brightness of light in the case of anisotropic scattering, which is the scattering of light in a medium in which the scattering particles are oriented in a preferred direction. (Anisotropic Scattering, Light, Physics).

hardcover. Zustand: Very Good. Very Good hardcover. Ex-library copy with the usual stamps and markings. 293 p.

Cloth. Zustand: Good. No Jacket.

Zustand: New. In.

Zustand: New. In.

Zustand: New.

Gebunden. Zustand: New.

Taschenbuch. Zustand: Neu. Radiation in a Cloudy Atmosphere | E. M. Feigelson | Taschenbuch | ix | Englisch | 2011 | Springer | EAN 9789400964457 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu.

Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Radiative heat transfer is a fundamental factor in the energetics of the terrestrial atmosphere: the system consisting of the atmosphere and the underlying layer is heated by the Sun, and this heating is compensated, on the average, by thermal radia tion. Only over a period of 1-3 days from some specified initial moment can the dynamic processes in the atmosphere be considered to be adiabatic. Global dynamic processes of long duration are regulated by the actual influxes of heat, one of the main ones being the radiative influx. Radiation must be taken into account in long-term, weather forecasting and when considering the global circulation of the atmosphere, the theory of climate, etc. Thus it is necessary to know the albedo of the system, the amount of solar radiation transmitted by the atmosphere, the absorptivity of the atmosphere vis-a-vis solar radiation, and also the effective radiation flux, the divergence of which represents the radiative cooling or heating. All these quantities have to be integrated over the wavelength spectrum of the solar or thermal radiation, and they must be ascertained as functions of the determining factors. The relation ships between the indicated radiation characteristics, the optical quantities directly determining them, the optically active compo nents of the atmosphere, and the meteorological fields will be discussed in this book.

Buch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Radiative heat transfer is a fundamental factor in the energetics of the terrestrial atmosphere: the system consisting of the atmosphere and the underlying layer is heated by the Sun, and this heating is compensated, on the average, by thermal radia tion. Only over a period of 1-3 days from some specified initial moment can the dynamic processes in the atmosphere be considered to be adiabatic. Global dynamic processes of long duration are regulated by the actual influxes of heat, one of the main ones being the radiative influx. Radiation must be taken into account in long-term, weather forecasting and when considering the global circulation of the atmosphere, the theory of climate, etc. Thus it is necessary to know the albedo of the system, the amount of solar radiation transmitted by the atmosphere, the absorptivity of the atmosphere vis-a-vis solar radiation, and also the effective radiation flux, the divergence of which represents the radiative cooling or heating. All these quantities have to be integrated over the wavelength spectrum of the solar or thermal radiation, and they must be ascertained as functions of the determining factors. The relation ships between the indicated radiation characteristics, the optical quantities directly determining them, the optically active compo nents of the atmosphere, and the meteorological fields will be discussed in this book.

Paperback. Zustand: Brand New. 308 pages. 9.25x6.10x0.70 inches. In Stock.

4to mayor. V pp, 245 pp. Encuadernación tela editorial con sobrecubierta ligeramente rozada en los bordes. Muy buen estado.