Titlebook: Microphysics of Clouds and Precipitation; H.R. Pruppacher,J.D. Klett Book 2010Latest edition Springer Science+Business Media B.V. 2010 Aer

Malevolent

書(shū)目名稱(chēng)Microphysics of Clouds and Precipitation影響因子(影響力)




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Obverse

The Structure of Water Substance,s and precipitation. The remaining chapters will be devoted to exploring how such particles come into being and how they grow. Understanding these processes depends, to a large extent, on knowledge of the physical properties of water vapor, water, ice, and, ultimately, on the physical characteristic

absorbed

palliate

向外供接觸

阻止

Homogeneous Nucleation,icle formation, since we did not come to grips with the crucial question of how a new phase is initiated. Consider, for example, that on the basis of the Kelvin equation alone, the formation of a water drop from homogeneous water vapor would be precluded because the vapor pressure required to hold a

母豬

The Atmospheric Aerosol and Trace Gases,haracteristics of the atmospheric aerosol. In dicussing this gaseous suspension of solid and liquid particles, it is customary to include all gases except water vapor, and all solid and liquid particles except hydrometeors, i.e., cloud and raindrops, and ice particles.

scrape

Heterogeneous Nucleation,rmation in homogeneous water vapor (see Chapter 7), do not occur in the atmosphere, but that typically supersaturations remain below 10% and most often even below 1%. This indicates that drop formation in the atmosphere occurs via heterogeneous nucleation involving aerosol particles (AP). Aerosol Pa

CODE

Hydrodynamics of Single Cloud and Precipitation Particles,e to the air. Sorne fraction of these particles will undergo complex hydrodynamic interactions causing sorne to collide. The particles will experience growth if the collision results in a permanent union. Generally in clouds, the time during which two colliding particles interact to form a single pa

FLIRT

Mechanics of the Atmospheric Aerosol,ffusion, sedimentation, and coagulation of aerosol particles, including sorne effects of turbulence. (Possible electrical influences will be discussed in Chapter 18.) We shall also extend and/or apply the various formulations to the problems of explaining sorne observed features of the size distribu