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Arthur D. Richmond
Researcher at National Center for Atmospheric Research
Publications - 262
Citations - 17782
Arthur D. Richmond is an academic researcher from National Center for Atmospheric Research. The author has contributed to research in topics: Ionosphere & Thermosphere. The author has an hindex of 67, co-authored 262 publications receiving 15605 citations. Previous affiliations of Arthur D. Richmond include University of California, Los Angeles & High Altitude Observatory.
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Journal ArticleDOI
In‐situ generated gravity waves as a possible seeding mechanism for equatorial spread‐F
David N. Anderson,Arthur D. Richmond,B. B. Balsley,Raymond G. Roble,Manfred A. Biondi,D. P. Sipler +5 more
TL;DR: In this article, the authors suggest that gravity waves may be generated in situ, via the wind shear mechanism, and show that wind shears may possibly generate gravity waves with horizontal wavelengths on the order of a few hundred kilometers.
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Intense dayside Joule heating during the 5 April 2010 geomagnetic storm recovery phase observed by AMIE and AMPERE
TL;DR: In this paper, the authors used data from the Active Magnetosphere and Planetary Electrodynamics Response Experiment (AMPERE) for the first time as an input to the Assimilative Mapping of Ionospheric Electrographysics (AMIE) algorithm, showing that during the recovery phase of the first storm there is intense ionospheric Joule heating in the dayside polar regions.
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Neutral wind influence on the electrodynamic coupling between the ionosphere and the magnetosphere
TL;DR: In this paper, the influence of the ionospheric wind dynamo on the steady state electrodynamic interaction between the ionosphere and the inner magnetosphere is evaluated with the Magnetosphere-Thermosphere-Ionosphere Electrodynamics General Circulation Model (MTIE-GCM) of Peymirat et al.
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Neutral wind effect in producing a storm time ionospheric additional layer in the equatorial ionization anomaly region
TL;DR: In this paper, a new type of additional layer is predicted to occur in the low-latitude F region ionosphere during evening hours of a major magnetic storm, which requires that storm time meridional neutral wind surges travel from high to low latitudes and cross into the opposite hemisphere.
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Analysis of thermospheric response to magnetospheric inputs
TL;DR: In this paper, the influence of the high-latitude energy inputs and heating distributions on the global thermosphere is investigated by coupling a new empirical model of the Poynting flux with the NCAR-TIEGCM.