Details

Autor(en) / Beteiligte

• Williams, E.R
• Watkins, G.W
• Blix, T.A
• Thrane, E.V
• Entzian, G
• von Cossart, G
• Greisiger, K.M
• Singer, W
• Taubenheim, J
• Friedrich, M
• Hall, C.M
• Katan, J.R
• Lastovicka, J
• de la Moreno, B.A
• Pakhomov, S.V
• Ranta, H
• Ts. Rapoport, Z
• Sinelnikov, V.M
• Samardjiev, D
• Nestorov, G
• Sauer, H.H
• Stauning, P

Titel

The ionosphere: morphology, development and coupling

Ist Teil von

• Journal of atmospheric and terrestrial physics, 1987, Vol.49 (7), p.777,789-787,808

Ort / Verlag

London: Elsevier B.V

Erscheinungsjahr

1987

Quelle

Elsevier Journal Backfiles on ScienceDirect (DFG Nationallizenzen)

Beschreibungen/Notizen

• The morphology of the MAP/WINE winter is examined, principally from ground-based and satellite observations. Winter anomaly is evident, occurring in bursts with a west to east shift in time. Auroral activity, particularly with reference to the times of major rocket salvoes, is generally low, with Andøya to the south of the auroral boundary in most cases. Minor stratospheric warmings, of which 4 occurred, are found to correlate with minima in radio wave absorption. Salvo R1 was launched during one of the minor warmings. Using data from a broad sector of Europe, coupling between the lower thermosphere and mesosphere is seen over large areas. Westerly winds are associated with high absorption (winter anomaly) and reversal to easterly winds with stratospheric warmings and low absorption. It is found possible to select cases, from amongst the MT series of rocket launchings, corresponding to quiet conditions, stratospheric warming, winter anomaly and particle precipitation in the general absence of other effects. Examining D- and lower E-region ionisation profiles for these caes it is found that, compared with a quiet night, the stratwarm night shows the lower E-region to have reduced ionisation. The ionisation ledge is of similar shape in all cases, but occurs over different height ranges. The observed effects all point to transport being a major factor and the need to measure vertical transport over the range of geophysical conditions examined is highlighted.