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000725640 019__ $$a908041798
000725640 020__ $$a9783319132693$$qelectronic book
000725640 020__ $$a3319132695$$qelectronic book
000725640 020__ $$z9783319132686
000725640 0247_ $$a10.1007/978-3-319-13269-3$$2doi
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000725640 08204 $$a551.57/6$$223
000725640 1001_ $$aSelvam, A. M.,$$eauthor.
000725640 24510 $$aRain formation in warm clouds$$h[electronic resource] :$$bgeneral systems theory /$$cA. M. Selvam.
000725640 264_1 $$aCham :$$bSpringer,$$c2015.
000725640 300__ $$a1 online resource (xv, 98 pages) :$$billustrations.
000725640 336__ $$atext$$btxt$$2rdacontent
000725640 337__ $$acomputer$$bc$$2rdamedia
000725640 338__ $$aonline resource$$bcr$$2rdacarrier
000725640 4901_ $$aSpringerBriefs in meteorology,$$x2199-9112
000725640 504__ $$aIncludes bibliographical references and index.
000725640 5050_ $$aGeneral Systems Theory Concepts in Atmospheric Flows -- Cumulus Cloud Model -- Universal Spectrum for Atmospheric Suspended Particulates: Comparison with Observations: Data set I -- Universal Spectrum for Atmospheric Suspended Particulates: Comparison with Observations: Data set II -- Universal Spectrum for Atmospheric Suspended Particulates: Comparison with Observations: Data set III.
000725640 506__ $$aAccess limited to authorized users.
000725640 520__ $$aThis book aims to promote the understanding of some of the basic mathematical and scientific issues in the subjects relating to climate dynamics, chaos and quantum mechanics. It is based on substantial research work in atmospheric science carried out over twenty years. Atmospheric flows exhibit self similar fractal fluctuations, a signature of long-range correlations on all space-time scales. Realistic simulation and prediction of atmospheric flows requires the incorporation of the physics of observed fractal fluctuation characteristics in traditional meteorological theory. A general systems theory model for fractal space-time fluctuations in turbulent atmospheric flows is presented and applied to the formation of rain in warm clouds. This model gives scale-free universal governing equations for cloud growth processes. The model predicted cloud parameters are in agreement with reported observations, in particular, the cloud drop-size distribution. Rain formation can occur in warm clouds within 30 minutes as observed in practice under favourable conditions of moisture supply in the environment. Traditional cloud physical concepts for rain development requires over an hour for a full-sized raindrop to form. The book provides background reading for postgraduate students of Meteorology, Atmospheric Sciences/Physics, Environmental Sciences, and scientists working in the field of the topic of the book as well as the multidisciplinary field of Nonlinear Dynamics and Chaos.
000725640 588__ $$aOnline resource; title from PDF title page (SpringerLink, viewed February 19, 2015).
000725640 650_0 $$aCloud physics.
000725640 650_0 $$aRain and rainfall.
000725640 77608 $$iPrint version:$$z9783319132686
000725640 830_0 $$aSpringerBriefs in meteorology.
000725640 852__ $$bebk
000725640 85640 $$3SpringerLink$$uhttps://univsouthin.idm.oclc.org/login?url=http://link.springer.com/10.1007/978-3-319-13269-3$$zOnline Access$$91397441.1
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000725640 983__ $$aOnline
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