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R. Gordon

Researcher at University College London

Publications -  7
Citations -  442

R. Gordon is an academic researcher from University College London. The author has contributed to research in topics: Thermosphere & Earth's magnetic field. The author has an hindex of 7, co-authored 7 publications receiving 441 citations.

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A theoretical and empirical study of the response of the high latitude thermosphere to the sense of the "Y" component of the interplanetary magnetic field

TL;DR: In this article, a three-dimensional, time-dependent global thermospheric model using a polar conversion electric field with a dependence on the Y component of the IMF to evaluate wind circulation is examined.
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A comparison of wind observations of the upper thermosphere from the dynamics explorer satellite with the predictions of a global time-dependent model

TL;DR: In this article, seven polar passes of the NASA Dynamics Explorer 2 (DE-2) satellite during October and early December 1981 have been used to examine the high-latitude circulation in the upper thermosphere.
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Modelling of thermospheric composition changes caused by a severe magnetic storm

TL;DR: In this article, the UCL 3-dimensional time-dependent thermospheric model with atomic and molecular components is used to study composition changes in the neutral gas at F-layer heights produced by a severe magnetic storm.
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The generation of vertical thermospheric winds and gravity waves at auroral latitudes—II. Theory and numerical modelling of vertical winds

TL;DR: In this article, the UCL three-dimensional, time-dependent thermospheric model was used to evaluate the effects of the geomagnetic energy and momentum sources in the presence of an auroral substorm.
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The westward thermospheric jet-stream of the evening auroral oval

TL;DR: In this article, the authors used ground-based and satellite observations to study the jet-streams of extreme magnitude in the vicinity of the auroral oval in the afternoon and evening period, and then evaluated with the aid of simulations using a global, three-dimensional, time-dependent model of thermospheric dynamics including the effects of magnetospheric convection and particle precipitation.