Propagation mechanism of very unusual low-latitude whistlers with additional traces of the earth-ionosphere waveguide propagation effect

1991 ◽  
Vol 39 (4) ◽  
pp. 611-616 ◽  
Author(s):  
S. Shimakura ◽  
M. Moriizumi ◽  
M. Hayakawa
2021 ◽  
Author(s):  
Yasmina Bouderba ◽  
Ener Aganou ◽  
Abdenaceur Lemgharbi

<p>In this work we will show the behavior of the horizontal component H of the Earth Magnetic Field (EMF) along the seasons during the period of solar cycle 24 lasting from 2009 to 2019. By means of  continuous measurements of geomagnetic components (X, Y) of the EMF, we compute the horizontal component H at the Earth’s surface. The data are recorded with a time resolution of one minute at Tamanrasset observatory in Algeria at the geographical coordinates of 22.79° North and 5.53° East. These data are available from the INTERMAGNET network. We find that the variation in amplitude of the hourly average of H component at low latitude changes from a season to another and it is greater at the maximum solar activity than at the minimum solar activity.</p><p><strong>Keywords:</strong> Solar cycle 24, Season, Horizontal component H. </p>


2010 ◽  
Vol 6 (S274) ◽  
pp. 40-43
Author(s):  
I. F. Shaikhislamov ◽  
Yu. P. Zakharov ◽  
V. G. Posukh ◽  
E. L. Boyarintsev ◽  
A. V. Melekhov ◽  
...  

AbstractIn previous experiments by the authors a generation of intense field aligned current (FAC) system on Terrella poles was observed. In the present report a question of these currents origin in a low latitude boundary layer of magnetosphere is investigated. Experimental evidence of such a link was obtained by measurements of magnetic field generated by tangential sheared drag. Results suggest that compressional and Alfven waves are responsible for FAC generation. The study is most relevant to FAC generation in the Earth and Hermean magnetospheres following pressure jumps in Solar Wind.


1981 ◽  
Vol 86 (A8) ◽  
pp. 6781 ◽  
Author(s):  
Masashi Hayakawa ◽  
Yoshihito Tanaka ◽  
Toshimi Okada ◽  
Akira Iwai

Radio Science ◽  
1992 ◽  
Vol 27 (2) ◽  
pp. 335-339 ◽  
Author(s):  
M. Hayakawa ◽  
S. Shimakura ◽  
M. Moriizumi ◽  
K. Ohta

Author(s):  
Kenji Ohta ◽  
Akio Shimizu ◽  
Masashi Hayakawa ◽  
Shin Shimakura

2012 ◽  
Vol 2012 ◽  
pp. 1-14 ◽  
Author(s):  
Sergey Pulinets

Ionospheric and atmospheric anomalies registered around the time of strong earthquakes in low-latitude regions are reported now regularly. Majority of these reports have the character of case studies without clear physical mechanism proposed. Here we try to present the general conception of low-latitude effects using the results of the recent author’s publications, including also rethinking the earlier results interpreted basing on recently established background physical mechanisms of anomalies generation. It should be underlined that only processes initiated by earthquake preparation are considered. Segregation of low-latitude regions for special consideration is connected with the important role of ionospheric equatorial anomaly in the seismoionospheric coupling and specific character of low-latitude earthquake initiated effects. Three main specific features can be marked in low-latitude ionospheric anomalies manifestation: the presence of magnetic conjugacy in majority of cases, local longitudinal asymmetry of effects observed in ionosphere in relation to the vertical projection of epicenter onto ionosphere, and equatorial anomaly reaction even on earthquakes outside equatorial anomaly (i.e., 30–40 LAT). The equality of effects morphology regardless they observed over land or over sea implies only one possible explanation that these anomalies are initiated by gaseous emanations from the Earth crust, and radon plays the major role.


2001 ◽  
Vol 28 (5) ◽  
pp. 801-806 ◽  
Author(s):  
O.P. Verkhoglyadova ◽  
A.V. Agapitov ◽  
V.N. Ivchenko

2013 ◽  
Vol 118 (6) ◽  
pp. 3692-3699 ◽  
Author(s):  
Brian S. Burkholder ◽  
Michael L. Hutchins ◽  
Michael P. McCarthy ◽  
Robert F. Pfaff ◽  
Robert H. Holzworth

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