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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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Expert Knowledge and Multivariate Emulation: The Thermosphere–Ionosphere Electrodynamics General Circulation Model (TIE-GCM)

TL;DR: This work demonstrates the use of the outer product emulator for efficient calculation, with an emphasis on predictive diagnostics for model choice and model validation, and uses the emulator to “verify” the underlying computer code and to quantify the qualitative physical understanding.

High-latitude energy input and its impact on the thermosphere

TL;DR: In this article, the authors present a quantitative assessment of high-latitude energy input and its partitioning in the polar cap by synthesizing various space and ground-based observations during the 17 January 2005 geomagnetic storm.
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On the day-to-day variation of the equatorial electrojet during quiet periods

TL;DR: In this article, the authors employ a numerical model introduced by Liu et al. (2013), which takes into account weather changes in the lower atmosphere and thus can reproduce ionospheric variability due to forcing from below.
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Atmospheric semidiurnal lunar tide climatology simulated by the Whole Atmosphere Community Climate Model

TL;DR: In this paper, the atmospheric semidiurnal lunar tide in surface pressure and zonal and meridional winds in the mesosphere and lower thermosphere (MLT) were simulated and compared with those from the Global Scale Wave Model (GSWM).
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Ground-based studies of ionospheric convection associated with substorm expansion

TL;DR: In this article, the instantaneous patterns of electric fields and currents in the high-latitude ionosphere are deduced by combining satellite and radar measurements of the ionospheric drift velocity, along with ground-based magnetometer observations for October 25, 1981.