Titlebook: Atmospheric Physics; J. V. Iribarne,H.-R. Cho Book 1980 D. Reidel Publishing Company 1980 Absorption.Cloud.Greenhouse effect.Precipitation

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ch as those related to the environ­ ment, have prompted the introduction of college and university courses in this field. There is consequently a need for good textbooks. A few appropriate books have appeared in the last few years, aimed at a variety of levels and having different orientations. Most

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https://doi.org/10.1007/978-3-658-31984-7w development of extensive layer clouds are indicative of a slow massive ascent of atmosphere, isolated clouds of large vertical development point to conditions of vertical instability, the approach of a cold front (cf. Ch. V I) is heralded by a whole succession of different types of clouds, etc.

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Radiation, λ and frequency .. These two quantities are related by .where c=velocity of light in vacuum=2.999 × 10.m/s. Electromagnetic waves carry energy, which may be absorbed by matter, producing different effects. This absorption can occur only in multiples of a . of energy, proportional to the frequency o

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Cloud Physics,al stability in the troposphere. The visible result of that ascent and condensation is of cource the formation of clouds; this is tantamount to saying that clouds often constitute visible indicators of vertical motions in the atmosphere. Thus the description and classification o clouds provide somet

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Atmospheric Electricity,igure 1a, held through an insulator. If there is a field ., there will be a polarization of charges, as indicated in the figure. Now let us connect the body and bring it into a Faraday cage attached to an electrometer (c). the instrument will show that the body is charged, as should be expected from

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Atmospheric Dynamics, first the nature of the forces experienced by the air before one can properly understand the complex ways through which air moves in the atmosphere. The air in the Earth’s atmosphere experiences basically four types of force, the pressure gradient force, the Coriolis force, and the frictional force

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