[PDF] Top 20 Equatorial scintillations in relation to the development of ionization anomaly
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Equatorial scintillations in relation to the development of ionization anomaly
... al.: Equatorial scintillations in relation to the development of ionization anomaly as irregular features of ionization in the upper atmosphere is ...phase ... See full document
14
Investigation of the response time of the equatorial ionosphere in context of the equatorial electrojet and equatorial ionization anomaly
... the relation [(C − T)/T] × ...the equatorial iono- sphere, which means the time taken by the EIA to respond to the changes in the primary zonal electric ... See full document
9
Multisatellite observations of an intensified equatorial ionization anomaly in relation to the northern Sumatra earthquake of March 2005
... the equatorial (±15 ◦ in geomagnetic latitude) electron density relative to the midlatitude density observed by the DEMETER satellite, also increased in the spatial and temporal vicinity of the earthquake ... See full document
20
Effect of solar and magnetic activity on VHF scintillations near the equatorial anomaly crest
... increases scintillations during win- ter (November–February) and near equinoxes (March–April; September–October), whereas it depresses the scintillations during the summer ...suppress scintillations ... See full document
12
Effect of solar and magnetic activity on VHF scintillations near the equatorial anomaly crest
... increases scintillations during win- ter (November–February) and near equinoxes (March–April; September–October), whereas it depresses the scintillations during the summer ...suppress scintillations ... See full document
13
Airglow observations over the equatorial ionization anomaly zone in Taiwan
... and development of these secondary depletions on the eastern wall, the primary depletion was drifting eastwards at a speed of 35–55 m s −1 ...the development of bifur- cation from the structuring of the ... See full document
9
Climatology and modeling of ionospheric scintillations and irregularity zonal drifts at the equatorial anomaly crest region
... of equatorial F-region E × B drifts is ...of equatorial plasma bubble irregularities and the distribution of ionospheric ionization at the crests of the EIA have possibly been affected during solar ... See full document
18
Characteristics of equatorial ionization anomaly (EIA) in relation to transionospheric satellite links around the northern crest in the Indian longitude sector
... post-sunset scintillations from a station Calcutta situated near the northern crest of EIA in the geophysically sensitive In- dian longitude ...band scintillations with S 4max ≥ ... See full document
7
Electrojet control of ambient ionization near the crest of the equatorial anomaly in the Indian zone
... in relation to time evolution of EEJ is reported till ...the equatorial anomaly, has been analyzed in conjunction with the EEJ data to make qualitative and quan- titative estimates of relative ... See full document
13
Solar control of ambient ionization of the ionosphere near the crest of the equatorial anomaly in the Indian zone
... the equatorial anomaly, reveals a good correspon- dence between the two when both are considered on a long- term ...short-term relation between TEC and solar ...the equatorial foun- tain ... See full document
11
Observations of equatorial ionization anomaly over Africa and Middle East during a year of deep minimum
... The literature above provides good knowledge of the EIA driven by the EEJ strength. The transportation of plasma to higher latitudes through the EIA phenomenon is well- known to relate with eastward electric field/EEJ ... See full document
10
Characteristics of the ionospheric total electron content of the equatorial ionization anomaly in the Asian-Australian region during 1996–2004
... the development of summer EIA crest should be retarded, and winter EIA crest should be ...of ionization is greater in the winter hemisphere due to dynamical transport increasing the O/N 2 ratio (Rishbeth, ... See full document
13
Variations in the total electron content near the crest of the equatorial ionization anomaly during the November 2004 geomagnetic storm
... It is evident from Fig. 3(a)–(c) that, on November 08, the VTEC was much lower than the quiet time mean VTEC. The variability in the difference of the two VTECs is due to the fact that the VTEC depends both on the local ... See full document
5
Variations in the equatorial ionization anomaly peaks in the Western Pacific region during the geomagnetic storms of April 6 and July 15, 2000
... EIA development on April 7 in Fig. 2 is the sup- pression of the equatorial plasma fountain due to a weaker eastward electric ...the equatorial region built by Fejer and Scherliess (1995) and the ... See full document
5
Spread F occurrence and drift under the crest of the equatorial ionization anomaly from continuous Doppler sounding and FORMOSAT 3/COSMIC scintillation data
... The GPS signal scintillation data obtained by radio occultation measurements onboard the F3/C satellite are consistent with the occurrences of OSSs in the Doppler data and show a similar seasonal and local time depend- ... See full document
18
GPS TEC Variation during Low to High Solar Activity Period (2010 2014) under the Northern Crest of Indian Equatorial Ionization Anomaly Region
... Abstract The measurements of ionospheric TEC (total electron content) are conducted at a low latitude Indian station Surat (21.16˚N, 72.78˚E Geog.), which lies un- der the northern crest of the equatorial ... See full document
24
Variability of ionospheric scintillation near the equatorial anomaly crest of the Indian zone
... ionospheric scintillations from the three locations with smaller latitudinal separation around the northern crest of equatorial anomaly and beyond reveals extreme variability, both in spatial and ... See full document
15
Effect of equatorial ionization anomaly on the occurrence of spread-F
... the equatorial ionosphere coupled with the E– W electric field causes the equatorial ionization anomaly (EIA) and equatorial spread-F ...to anomaly crest region ... See full document
8
Quasi-16-day periodic meridional movement of the equatorial ionization anomaly
... Fig. 9. L–S periodogram of the location of EIA peak in East Asia and South American longitude during this SSW. of EIA crest exhibit a weak or unidentified quasi-16-day vari- ation. The 16-day periodic component does not ... See full document
11
Nonmigrating tidal signatures in the magnitude and the inter-hemispheric asymmetry of the equatorial ionization anomaly
... obtained amplitudes and phases of the synthetic tidal com- ponents are list in Table 3. As expected, during the months around August DE3 is the dominating tidal component for the WN4 structure of the CTR, exceeding the ... See full document
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