Night–side effects on the polar ionospheric convection due to a solar wind pressure impulse

The Sudden Impulse (SI) of solar wind dynamic pressure of 20 february 2000, 21:03 UT, is investigated by making use of data from WIND, GEOTAIL, POLAR and GOES; ground magnetometer chains (Greenland, IMAGE, CANOPUS); SuperDARN HF radars in both Northern and Southern hemispheres. The main effect of th...

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Bibliographic Details
Main Authors: Coco, Igino, Amata, Ermanno, Marcucci, Maria Federica, Villain, Jean-Paul, Hanuise, Christian, Cerisier, Jean-Claude, St. Maurice, Jean-Pierre, Sato, Natsuo
Other Authors: Istituto Nazionale di Astrofisica – Istituto di Fisica dello Spazio Interplanetario, Via Fosso del Cavaliere 100, 00133 Roma, Italy, Centre Nationale de la Recherche Scientifique – Laboratoire de Physique et Chimie de l’Environnement, Orleans, France, Institut “Pierre Simon Laplace” – Centre d’Etudes des Environnements Terrestre et Planetaires, Saint–Maur des Fossees, France, University of Saskatchewan – Department of Physics and Engineering Physics, Saskatoon, Canada, National Institute of Polar Research – Tokyo, Japan
Format: Article in Journal/Newspaper
Language:English
Published: 2006
Subjects:
Online Access:http://hdl.handle.net/2122/10829
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Summary:The Sudden Impulse (SI) of solar wind dynamic pressure of 20 february 2000, 21:03 UT, is investigated by making use of data from WIND, GEOTAIL, POLAR and GOES; ground magnetometer chains (Greenland, IMAGE, CANOPUS); SuperDARN HF radars in both Northern and Southern hemispheres. The main effect of the SI described herein is an enhancement of the ionospheric convection around midnight MLT. We suggest that such an enhancement be due to an increase of the dawn–dusk electric field caused by the SI compression of the magnetospheric tail. Published 91-93 2A. Fisica dell'alta atmosfera N/A or not JCR