Microphysics of Clouds and PrecipitationSpringer Science & Business Media, 25.06.2010 - 954 Seiten Cloud physics has achieved such a voluminous literature over the past few decades that a significant quantitative study of the entire field would prove unwieldy. This book concentrates on one major aspect: cloud microphysics, which involves the processes that lead to the formation of individual cloud and precipitation particles. Common practice has shown that one may distinguish among the following addi tional major aspects: cloud dynamics, which is concerned with the physics respon sible for the macroscopic features of clouds; cloud electricity, which deals with the electrical structure of clouds and the electrification processes of cloud and precipi tation particles; and cloud optics and radar meteorology, which describe the effects of electromagnetic waves interacting with clouds and precipitation. Another field intimately related to cloud physics is atmospheric chemistry, which involves the chemical composition ofthe atmosphere and the life cycle and characteristics of its gaseous and particulate constituents. In view of the natural interdependence of the various aspects of cloud physics, the subject of microphysics cannot be discussed very meaningfully out of context. Therefore, we have found it necessary to touch briefly upon a few simple and basic concepts of cloud dynamics and thermodynamics, and to provide an account of the major characteristics of atmospheric aerosol particles. We have also included a separate chapter on some of the effects of electric fields and charges on the precipitation-forming processes. |
Inhalt
| 1 | |
| 10 | |
CHAPTER 3 THE STRUCTURE OF WATER SUBSTANCE | 74 |
CHAPTER 4 EQUILIBRIUM BETWEEN WATER VAPOR WATEIt AQUEOUSSOLUTIONS AND ICE IN BULK | 100 |
CHAPTER 5 SURFACE PROPERTIES OF WATER SUBSTANCE | 126 |
CHAPTER 6 EQUILIBRIUM BEHAVIOR OF CLOUD DROPS AND ICEPARTICLES | 167 |
CHAPTER 7 HOMOGENEOUS NUCLEATION | 191 |
CHAPTER 8 THE ATMOSPHERIC AEROSOL AND TRACE GASES | 216 |
CHAPTER 13 DIFFUSION GROWTH AND EVAPORATION OF WATER DROPSAND SNOW CRYSTALS | 502 |
CHAPTER 14 CLOUD PARTICLE INTERACTIONS | 568 |
CHAPTER 15 GROWTH OF CLOUD DROPS BY COLLISION COALESCENCEAND BREAKUP | 617 |
CHAPTER 16 GROWTH OF ICE PARTICLES BY ACCRETION AND ICEPARTICLE MELTING | 659 |
CHAPTER17 CLOUD CHEMISTRY | 700 |
CHAPTER 18 CLOUD ELECTRICITY | 792 |
APPENDICES | 853 |
REFERENCES | 874 |
CHAPTER 9 HETEROGENEOUS NUCLEATION | 287 |
CHAPTER 10 HYDRODYNAMICS OF SINGLE CLOUD AND PRECIPITATIONPARTICLES | 361 |
CHAPTER Il MECHANICS OF THE ATMOSPHERIC AEROSOL | 447 |
CHAPTER 12 COOLING OF MOIST AIR | 485 |
LIST OF PRINCIPAL SYMBOLS | 935 |
TABLE OF PHYSICAL CONSTANTS | 944 |
| 945 | |
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adsorption aerosol particles assumed Atmos atmosphere Beard breakup charge Chem cloud base cloud drops cm² cm³ coagulation coalescence coefficient collision efficiency computed condensation constant curve decreasing density diameter diffusion distribution DROP RADIUS droplets effect electric field energy entrainment Environ equation equilibrium experimental fall Figure flow freezing function Geophys given graupel hailstones heat Heymsfield Hobbs ice crystals ice nucleation ice particle increasing interface ions Junge larger layer liquid water content Mason mass mechanism Meteor mole nucleation number concentration oblate spheroid observed obtained phase Phys ppbv pressure Pruppacher Quart raindrops ratio relative humidity Reynolds number riming saturation scavenging Section Seinfeld snow crystals solution drop spectrum sphere spherical spheroid Stokes Stokes flow studies substrate supercooled supercooled water supersaturation surface temperature terminal velocity troposphere turbulent values variation water drops water molecules water vapor µm radius
