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Gradient-Induced Errors

Published in Geophysical monograph • Mar 20, 2013
NobleIDNI5P30W42R39S09
Authors:
N. Hershkowitz
,
D. Diebold

Abstract

Plasma gradients are a possible source of error in the measurement of weak double layers in the magnetosphere by satellite double probes. Space charge enhancement of Plasma Gradient Induced Error (PGIE) has been considered elsewhere [Diebold et al., 1994] and is briefly reviewed here. Possible effec...

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