A study of the relation between ionospheric absorption and predicted HF propagation parameters at high latitudes

Author(s):  
V. Jodalen
Radio Science ◽  
1991 ◽  
Vol 26 (4) ◽  
pp. 1017-1024 ◽  
Author(s):  
M. H. Reilly ◽  
F. J. Rhoads ◽  
J. M. Goodman ◽  
M. Singh

2016 ◽  
Vol 57 (3) ◽  
pp. 821-834 ◽  
Author(s):  
D.V. Blagoveshchensky ◽  
O.A. Maltseva ◽  
M.M. Anishin ◽  
D.D. Rogov ◽  
M.A. Sergeeva

1976 ◽  
Vol 38 (12) ◽  
pp. 1289-1297 ◽  
Author(s):  
J Vassal ◽  
J.J Berthelier ◽  
J Lavergnat ◽  
M Sylvain

2018 ◽  
Author(s):  
Donat Blagoveshchensky ◽  
Olga Maltseva ◽  
Tatyana Nikitenko ◽  
Gennady Zhbankov

1967 ◽  
Vol 31 ◽  
pp. 265-278 ◽  
Author(s):  
A. Blaauw ◽  
I. Fejes ◽  
C. R. Tolbert ◽  
A. N. M. Hulsbosch ◽  
E. Raimond

Earlier investigations have shown that there is a preponderance of negative velocities in the hydrogen gas at high latitudes, and that in certain areas very little low-velocity gas occurs. In the region 100° <l< 250°, + 40° <b< + 85°, there appears to be a disturbance, with velocities between - 30 and - 80 km/sec. This ‘streaming’ involves about 3000 (r/100)2solar masses (rin pc). In the same region there is a low surface density at low velocities (|V| < 30 km/sec). About 40% of the gas in the disturbance is in the form of separate concentrations superimposed on a relatively smooth background. The number of these concentrations as a function of velocity remains constant from - 30 to - 60 km/sec but drops rapidly at higher negative velocities. The velocity dispersion in the concentrations varies little about 6·2 km/sec. Concentrations at positive velocities are much less abundant.


2000 ◽  
Vol 179 ◽  
pp. 201-204
Author(s):  
Vojtech Rušin ◽  
Milan Minarovjech ◽  
Milan Rybanský

AbstractLong-term cyclic variations in the distribution of prominences and intensities of green (530.3 nm) and red (637.4 nm) coronal emission lines over solar cycles 18–23 are presented. Polar prominence branches will reach the poles at different epochs in cycle 23: the north branch at the beginning in 2002 and the south branch a year later (2003), respectively. The local maxima of intensities in the green line show both poleward- and equatorward-migrating branches. The poleward branches will reach the poles around cycle maxima like prominences, while the equatorward branches show a duration of 18 years and will end in cycle minima (2007). The red corona shows mostly equatorward branches. The possibility that these branches begin to develop at high latitudes in the preceding cycles cannot be excluded.


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