Extrapolating EISCAT Pedersen conductances to other parts of the sky using groundbased TV auroral images
Abstract. Ionospheric conductivity is not very easily measured directly. Incoherent scatter radars perhaps o€er the best method but can only measure at one point in the sky at any one time and are limited in their time resolution. Statistical models of average conductivity are available but these ma...
| Main Authors: | , , |
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| Format: | Text |
| Language: | English |
| Published: |
1998
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.371.7003 http://hal.archives-ouvertes.fr/docs/00/31/63/93/PDF/angeo-16-583-1998.pdf |