New PDF release: A Short Course in Cloud Physics

By M.K. Yau, R R Rogers

ISBN-10: 0750632151

ISBN-13: 9780750632157

Covers crucial elements of cloud and precipitation physics and has been generally rewritten with over 60 new illustrations and lots of new and recent references. Many present themes are lined akin to mesoscale meteorology, radar cloud reviews and numerical cloud modelling, and themes from the second one version, similar to serious storms, precipitation approaches and big scale features of cloud physics, were revised. difficulties are integrated as examples and to complement the text.

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Additional resources for A Short Course in Cloud Physics

Sample text

Geopotential The geopotential efz) is defined as the potential energy of a unit mass at height z above a reference level, usually mean sea level. By this definition, dljJ = gdz is the increase in geopotential for an incremental increase in altitude. Thus there is a close relation between the geopotential at level z and the geometric altitude. 8 m/s2 , and g is the average value of g between sea level and height z. Meteorological thermodynamic charts such as the tephigram usually have altitude scales, which are derived from the relation between the height in geopotential meters and the pressure in a standard atmosphere.

The magnitude of this force, called the Coriolis force, is equal to twice the product of the local rate of rotation and the speed of the object. Applying this result to the movement of an air parcel in the northern hemisphere, we see that the Coriolis force acts in a direction normal to the trajectory of the parcel and tends to deflect it toward the right. Let x denote the eastward direction and y the northward direction. 29 x 10- 5 rad/s), 11 is the latitude, and u and v are the x and y components of the horizontal wind.

The values of latent heat were taken from the 6th edition (R. J. List, 1951) of the Smithsonian Meteorological Tables. 17) where es is in mb and T is in degrees C. Moist air: its vapor content Atmospheric air is a mixture of dry air and water vapor. There are different ways to describe the vapor content, depending on the application. (a) (b) (c) of dry Vapor pressure e, the partial pressure of the water vapor. 1). Mixing ratio w, defined as the mass of water vapor per unit mass air. d. d = (p - e)IR'Tso that W W = e = £-.

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A Short Course in Cloud Physics by M.K. Yau, R R Rogers

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