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William H. Hooke
Researcher at American Meteorological Society
Publications - 39
Citations - 1872
William H. Hooke is an academic researcher from American Meteorological Society. The author has contributed to research in topics: Ionosphere & Wave propagation. The author has an hindex of 15, co-authored 38 publications receiving 1779 citations. Previous affiliations of William H. Hooke include Silver Spring Networks & Environmental Science Services Administration.
Papers
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Waves in the atmosphere
TL;DR: In this paper, the authors propose a method to solve the problem of how to find the shortest path between two points of interest in a set of images. Index Reference Record created on 2004-09-07, modified on 2016-08-08
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Ionospheric irregularities produced by internal atmospheric gravity waves
TL;DR: In this article, a perturbation treatment is used to determine the nature and magnitude of the effects of internal atmospheric gravity waves on the ambient rates of production, chemical loss, and motion of the ionization.
Book
Waves in the atmosphere : atmospheric infrasound and gravity waves : their generation and propagation
TL;DR: In this paper, the authors provide an introduction to the theory of propagation and the dynamics of mesoscale atmospheric masses and wave propagation in the field of radiophysics, as well as their role in the generation of clear air turbulence (CAT).
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The ionospheric response to internal gravity waves: 1. The F2 region response
TL;DR: In this paper, the F2 region ionospheric response to individual internal gravity waves is calculated as a function of the azimuth of wave propagation, and the response is shown to be highly anisotropic, with the anisotropy itself depending on the wave parameters, the geomagnetic dip and the prevailing ionization density gradient.
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Estimating the Depth of the Daytime Convective Boundary Layer
J. C. Kaimal,N. L. Abshire,R. B. Chadwick,M. T. Decker,William H. Hooke,Robert A. Kropfli,William Neff,F. Pasqualucci,Peter H. Hildebrand +8 more
TL;DR: In this paper, three in-situ and five remote sensing techniques for measuring the height of the daytime convective boundary layer were compared, and good agreement between the different systems when the capping inversion was steep and well defined, and some variability when the stratification was not so sharply defined.