Daytime verticalE×Bdrift velocities inferred from ground-based magnetometer observations at low latitudes
Author:
Affiliation:
1. Cooperative Institute for Research in Environmental Sciences; University of Colorado and Space Environment Center, National Oceanic and Atmospheric Administration; Boulder Colorado USA
2. Radio Observatorio de Jicamarca; Lima Peru
Publisher
American Geophysical Union (AGU)
Subject
Atmospheric Science
Reference26 articles.
1. Anderson , D. N. J. A. Klobuchar P. H. Doherty R. G. Rastogi 1992 A comparison of theoretical modeling of the low latitude ionosphere against TEC data from the Indian longitudes during solar minimum International Beacon Symposium Boston, Mass.
2. Estimating daytime vertical E × B drift velocities in the equatorial F-region using ground-based magnetometer observations;Anderson;Geophys. Res. Lett.,2002
3. Evidence of a stratified echoing region at 150 kilometers in the vicinity of the magnetic equator during daylight hours;Balsley;J. Geophys. Res.,1964
4. Kilometric irregularities in the E and F regions of the daytime equatorial ionosphere observed by a high resolution HF radar;Blanc;Geophys. Res. Lett.,1996
5. Chau , J. L. 1998 Examination of various techniques for measuring wind velocities using clear-air radars, with emphasis on vertical wind measurements Univ. of Colo. Boulder
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