Crynodeb
Wind variations in the lower and upper thermosphere have been compared during a magnetic quiet period. The mesosphere/lower thermosphere and thermospheric F-regions are dynamically coupled through thermospheric winds, tides and waves. The regular fluctuations in the earth's magnetic field on quiet days are caused by dynamo-induced currents which flow in the ionosphere/thermosphere system. This paper presents simultaneous mesosphere/lower thermosphere and upper thermospheric region wind observations during a quiet magnetic period using data from TIMED and CHAMP satellites. The upper thermospheric winds from two time local sectors are observed to be faster than the lower thermospheric winds
| Iaith wreiddiol | Saesneg |
|---|---|
| Teitl | PROCEEDINGS OF SAIP2012: THE 57TH ANNUAL CONFERENCE OF THE SOUTH AFRICAN INSTITUTE OF PHYSICS |
| Golygyddion | J. J. VanRensburg |
| Cyhoeddwr | South African Institute of Physics |
| Tudalennau | 392-398 |
| Nifer y tudalennau | 7 |
| Statws | Cyhoeddwyd - 2012 |
| Digwyddiad | 57th Annual Conference of the South-African-Institute-of-Physics (SAIP) - Pretoria, De Affrica Hyd: 09 Gorff 2012 → 13 Gorff 2012 |
Cynhadledd
| Cynhadledd | 57th Annual Conference of the South-African-Institute-of-Physics (SAIP) |
|---|---|
| Gwlad/Tiriogaeth | De Affrica |
| Dinas | Pretoria |
| Cyfnod | 09 Gorff 2012 → 13 Gorff 2012 |