scholarly journals Correction to “On the utilization of ionosonde data to analyze the latitudinal penetration of ionospheric storm effects”

1988 ◽  
Vol 15 (5) ◽  
pp. 542-542 ◽  
Author(s):  
Jeffrey M. Forbes ◽  
Mihail Codrescu ◽  
Timothy J. Hall
Keyword(s):  
Ionospheric Storm ◽  
Storm Effects

scholarly journals Positive and negative GPS-TEC ionospheric storm effects during the extreme space weather event of March 2015 over the Brazilian sector

2016 ◽  
Vol 121 (6) ◽  
pp. 5613-5625 ◽  
Author(s):  
P. R. Fagundes ◽  
F. A. Cardoso ◽  
B. G. Fejer ◽  
K. Venkatesh ◽  
B. A. G. Ribeiro ◽  
...  
Keyword(s):  
Space Weather ◽  
Ionospheric Storm ◽  
Weather Event ◽  
Storm Effects ◽  
Gps Tec ◽  
Space Weather Event

Some ionospheric storm effects at an antarctic station

2016 ◽  
Vol 57 (6) ◽  
pp. 1319-1327 ◽  
Author(s):  
Gustavo A. Mansilla ◽  
Marta M. Zossi
Keyword(s):  
Ionospheric Storm ◽  
Storm Effects

scholarly journals Modeling investigation of ionospheric storm effects over Millstone Hill during August 4–5, 1992

2004 ◽  
Vol 56 (9) ◽  
pp. 903-908 ◽  
Author(s):  
Jiuhou Lei ◽  
Libo Liu ◽  
Weixing Wan ◽  
Shun-Rong Zhang
Keyword(s):  
Ionospheric Storm ◽  
Storm Effects

scholarly journals Positive ionospheric storm effects at Latin America longitude during the superstorm of 20–22 November 2003: revisit

2012 ◽  
Vol 30 (5) ◽  
pp. 831-840 ◽  
Author(s):  
B. Zhao ◽  
W. Wan ◽  
J. Lei ◽  
Y. Wei ◽  
Y. Sahai ◽  
...  
Keyword(s):  
Latin America ◽  
Electron Density ◽  
Topside Ionosphere ◽  
Electron Content ◽  
South American ◽  
Ionospheric Storm ◽  
The South ◽  
Total Electron ◽  
Storm Effects ◽  
Low Latitudes

Abstract. Positive ionospheric storm effects that occurred during the superstorm on 20 November 2003 are investigated using a combination of ground-based Global Positioning System (GPS) total electron content (TEC), and the meridian chain of ionosondes distributed along the Latin America longitude of ~280° E. Both the ground-based GPS TEC and ionosonde electron density profile data reveal significant enhancements at mid-low latitudes over the 280° E region during the main phase of the November 2003 superstorm. The maximum enhancement of the topside ionospheric electron content is 3.2–7.7 times of the bottomside ionosphere at the locations of the ionosondes distributed around the mid- and low latitudes. Moreover, the height of maximum electron density exceeds 400 km and increases by 100 km compared with the quiet day over the South American area from middle to low latitudes, which might have resulted from a continuous eastward penetration electric field and storm-generated equatorward winds. Our results do not support the conclusions of Yizengaw et al. (2006), who suggested that the observed positive storm over the South American sector was mainly the consequence of the changes of the bottomside ionosphere. The so-called "unusual" responses of the topside ionosphere for the November 2003 storm in Yizengaw et al. (2006) are likely associated with the erroneous usage of magnetometer and incomplete data.

Ionospheric storm effects at subauroral latitudes: A case study

1991 ◽  
Vol 96 (A2) ◽  
pp. 1275-1288 ◽  
Author(s):  
G. W. Prölss ◽  
L. H. Brace ◽  
H. G. Mayr ◽  
G. R. Carignan ◽  
T. L. Killeen ◽  
...  
Keyword(s):  
Ionospheric Storm ◽  
Storm Effects

Perturbations of the FUV dayglow and ionospheric storm effects

1998 ◽  
Vol 22 (1) ◽  
pp. 129-134 ◽  
Author(s):  
G.W. Prölss ◽  
J.D. Craven
Keyword(s):  
Ionospheric Storm ◽  
Storm Effects
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