By Carmen J. Nappo

ISBN-10: 0123852234

ISBN-13: 9780123852236

Gravity waves exist in all kinds of geophysical fluids, corresponding to lakes, oceans, and atmospheres. They play a major position in redistributing power at disturbances, corresponding to mountains or seamounts and they're normally studied in meteorology and oceanography, quite simulation types, atmospheric climate versions, turbulence, pollution, and weather examine. An advent to Atmospheric Gravity Waves offers readers with a operating heritage of the basic physics and arithmetic of gravity waves, and introduces a large choice of functions and diverse contemporary advances. Nappo offers a concise quantity on gravity waves with a lucid dialogue of present observational options and instrumentation.An accompanying website includes genuine information, machine codes for info research, and linear gravity wave types to additional improve the reader's knowing of the book's material.

  • Companion site positive aspects animations and streaming video
  • Foreword via George Chimonas, a well known specialist at the interactions of gravity waves with turbulence
  • Includes a brand new application-based part to be used in weather and climate predictions
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    Extra info for An Introduction to Atmospheric Gravity Waves

    Example text

    9 Sketch of a hypothetical experiment of flow over an obstacle. 10 Illustration of the difference between flow momentum (a) and pseudomomentum (b). Values are in kg ms−1 . Taken from Durran (1995). (a) the waves had momentum equal to their pseudo-momentum, Ek/ , and (b) the medium were absent. Statements (a) and (b) constitute the McIntyre’s pseudo-momentum rule. 10 taken from Durran (1995) illustrates the difference between momentum and pseudo-momentum in the case of a mountain wave. 10a shows contours of perturbation horizontal momentum, ρu − ρ¯ u, ¯ and Fig.

    42) critical levels will have to be considered if they are present. The treatment of critical levels is given later in Chapter 5. 42) be constant. These plane wave solutions in physical space will have the form z/2Hs i(kx−ωt) ˆ e . 58) an alternate form is ˆ w1 (x, z, t) = w(z) ρs ρ0 (z) 1/2 ei(kx−ωt) . 46) we see that if the wave fronts move upward, then the background air density seen by the wave, ρ0 , decreases. 46), this means that the wave amplitude, w1 , increases with height. , ρ0 u 1 w1 = 1 λ λ ρ0 u 1 w1 dx.

    Further discussions of pseudo-momentum and pseudo-energy can be found for example in Andrews and McIntyre (1978), Dunkerton (1981), Held (1985), Tanaka (1996), Durran (1995), Lott (1998), and Fritts and Alexander (2003). 55 PROBLEMS PROBLEMS 1. In an calm isothermal atmosphere with a temperature of 280 K, a gravity wave with wavelength 25 km and phase speed 15 ms−1 propagates upward at an angle of 48◦ to the horizontal. The amplitude of w1 is 1 ms−1 . Calculate the amplitudes of u 1 , θ1 , and p1 .

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    An Introduction to Atmospheric Gravity Waves by Carmen J. Nappo

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