TY - JOUR
T1 - An analysis of the scale height at the F2-layer peak over three middle-latitude stations in the European sector
AU - Mosert, M.
AU - Buresova, D.
AU - Magdaleno, S.
AU - de la Morena, B.
AU - Altadill, D.
AU - Ezquer, R. G.
AU - Scida, L.
PY - 2013
Y1 - 2013
N2 - This paper presents the results of an analysis of the variations of the scale height at the F-2-layer peak (H-m) under different seasonal and solar-activity conditions. The database includes hourly H-m values derived from ionograms recorded at three middle-latitude stations in the European sector: El Arenosillo (37.1 degrees N; 353.3 degrees E), Ebro (40.8 degrees N, 0.5 degrees E) and Pruhonice (50.0 degrees N; 15.0 degrees E). The results show that, in general: (1) H-m exhibits diurnal variation with higher values during daytime than during night-time and secondary peaks around sunrise and sunset; (2) during winter time the scale height is lower than in summer time; (3) the scale heights increase with increasing solar activity; (4) H-m decreases when the latitude increases; (5) H-m shows a low correlation with the F-2-region peak parameters NmF2 and h(m)F(2) and a high correlation with the thickness parameter B-0 and the equivalent slab thickness E-ST; (6) the day-to-day variability is greater at low solar activity than at high solar activity-it reaches maximum values around sunrise or sunset and it is lower around midnight than around noon at low solar activity. The results of this study are similar to those reported by other authors and can be useful for estimating the topside ionosphere from bottomside measurements and modelling.
AB - This paper presents the results of an analysis of the variations of the scale height at the F-2-layer peak (H-m) under different seasonal and solar-activity conditions. The database includes hourly H-m values derived from ionograms recorded at three middle-latitude stations in the European sector: El Arenosillo (37.1 degrees N; 353.3 degrees E), Ebro (40.8 degrees N, 0.5 degrees E) and Pruhonice (50.0 degrees N; 15.0 degrees E). The results show that, in general: (1) H-m exhibits diurnal variation with higher values during daytime than during night-time and secondary peaks around sunrise and sunset; (2) during winter time the scale height is lower than in summer time; (3) the scale heights increase with increasing solar activity; (4) H-m decreases when the latitude increases; (5) H-m shows a low correlation with the F-2-region peak parameters NmF2 and h(m)F(2) and a high correlation with the thickness parameter B-0 and the equivalent slab thickness E-ST; (6) the day-to-day variability is greater at low solar activity than at high solar activity-it reaches maximum values around sunrise or sunset and it is lower around midnight than around noon at low solar activity. The results of this study are similar to those reported by other authors and can be useful for estimating the topside ionosphere from bottomside measurements and modelling.
KW - Middle-latitude ionosphere
KW - alpha-Chapman scale height
KW - Bottom density profile
UR - https://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=pure_univeritat_ramon_llull&SrcAuth=WosAPI&KeyUT=WOS:000307224500010&DestLinkType=FullRecord&DestApp=WOS_CPL
U2 - 10.5047/eps.2011.04.013
DO - 10.5047/eps.2011.04.013
M3 - Article
VL - 64
SP - 493
EP - 503
JO - Earth Planets and Space
JF - Earth Planets and Space
IS - 6
ER -