An Introduction to Atmospheric Physics - download pdf or read online

By David G. Andrews

ISBN-10: 0521693187

ISBN-13: 9780521693189

A quantitative creation to the Earth's surroundings for intermediate-advanced undergraduate and graduate scholars, with an emphasis on underlying actual ideas. This variation has been introduced thoroughly up to date, and now incorporates a new bankruptcy at the physics of weather switch which builds upon fabric brought in past chapters, giving the scholar a extensive knowing of a few of the actual thoughts underlying this most vital and topical topic. unlike many different books on atmospheric technological know-how, the emphasis is at the underlying physics. Atmospheric functions are built typically within the difficulties given on the finish of every bankruptcy. The booklet is a necessary source for all scholars of atmospheric physics as a part of an atmospheric technology, meteorology, physics, Earth technology, planetary technological know-how, or utilized arithmetic direction.

Show description

Read Online or Download An Introduction to Atmospheric Physics PDF

Best weather books

Limiting the Magnitude of Future Climate Change (America's - download pdf or read online

Weather swap, pushed by way of the expanding focus of greenhouse gases within the surroundings, poses severe, wide-ranging threats to human societies and traditional ecosystems around the globe. the most important total resource of greenhouse gasoline emissions is the burning of fossil fuels. the worldwide atmospheric focus of carbon dioxide, the dominant greenhouse gasoline of shock, is expanding by way of approximately components in keeping with million consistent with yr, and the us is presently the second-largest contributor to worldwide emissions in the back of China.

Download e-book for kindle: Atmospheric Turbulence, Meteorological Modeling and by Peter R. Lang, Frank S. Lombargo

Turbulence is a fluid regime characterized through chaotic, stochastic estate adjustments. This contains low momentum diffusion, excessive momentum convection, and fast version of strain and pace in area and time. This booklet will provide the reader new insights into this ordinary phenomenon that happens daily but is a puzzle that's not but absolutely resolved in classical physics.

Download PDF by Jack Williams: The AMS Weather Book: The Ultimate Guide to America’s

The US has essentially the most different and dynamic climate on the earth. each year, the Gulf Coast is battered through hurricanes, the good Plains are ravaged through tornados, the Midwest is pummeled by way of blizzards, and the temperature within the Southwest reaches a sweltering a hundred and twenty levels. severe climate could be a topic of existence and demise, yet even if it truly is pleasant—72 levels and sunny—weather continues to be valuable to the lives of all americans.

Additional info for An Introduction to Atmospheric Physics

Sample text

For typical atmospheric values of T and μs it is found that s ≤ a . 11. Note that s depends on 39 The saturated adiabatic lapse rate the temperature and pressure, through its dependences on T and μs (T, p). 49) say. 49) are called saturated adiabatics. Given the expression for s and suitable starting values of T and p, they may readily be calculated numerically. 5 relating to the static stability of a region of the atmosphere can now be extended to allow for the effects of moisture. In particular, it follows that, if the actual lapse rate is less than the SALR s , then the region is statically stable even if the air is saturated.

8. 1 hPa. 09Vl (unlike most substances, water expands on freezing) and the specific volume of water vapour is Vv ≈ 2 × 105 Vl . 35) of the Clausius–Clapeyron equation applies to each of these transitions. 38); indeed, since the two latent heats are fairly similar in size, the two curves are quite close. 37 The saturated adiabatic lapse rate Fig. 8 The phase transitions between ice, liquid water and water vapour. The triple point is indicated by the small solid circle. 4 × 105 hPa K−1 near the triple point.

18) where H = U + pV is the enthalpy. 18) involve functions of state, they apply both for reversible and for irreversible changes. 19) also hold. 20) where cv is the specific heat capacity at constant volume and is independent of T. 21) where cp = cv + Ra is the specific heat capacity of air at constant pressure. 18), we get T δS = cp δT − Ra T δp. 24) where κ = Ra /cp , which is approximately 27 for a diatomic gas, and S0 is a constant. An adiathermal process is one in which heat is neither gained nor lost, so that δQ = 0.

Download PDF sample

An Introduction to Atmospheric Physics by David G. Andrews

by Ronald

Rated 4.62 of 5 – based on 27 votes