Ionospheric Signatures During G2, G3 and G4 Storms in Mid‐Latitude-Reference-Cited by-同舟云学术

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Ionospheric Signatures During G2, G3 and G4 Storms in Mid‐Latitude

Published:2022-05 Issue:5 Volume:57 Page:
ISSN:0048-6604
Container-title:Radio Science
language:en
Short-container-title:Radio Science

Author:

Dahal Subodh¹^ORCID,Adhikari Binod²^ORCID,Khadka Anil Kumar¹,Silwal Ashok³,Gupta Suresh Prasad⁴,Chapagain Narayan Prasad⁵^ORCID

Affiliation:

1. Central Department of Physics Kirtipur Nepal

2. St. Xavier's College, Maitighar Kathmandu Nepal

3. Department of Space Science University of Alabama in Huntsville Huntsville AL USA

4. Department of Physics Patan Multiple Campus Tribhuvan University Kathmandu Nepal

5. Amrit Science Campus Tribhuvan University Kathmandu Nepal

Publisher

American Geophysical Union (AGU)

Subject

Electrical and Electronic Engineering,General Earth and Planetary Sciences,Condensed Matter Physics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022RS007430

Reference68 articles.

1. The role of the ring current in the generation or inhibition of equatorialFlayer irregularities during magnetic storms

2. Equatorial spread F/plasma bubble irregularities under storm time disturbance electric fields

3. Abdu M. A. De Souza J. R. Sobral J. H. A. &Batista I. S.(2006).Magnetic storm associated disturbance dynamo effects in the low and equatorial latitude ionosphere. Geophysical Monograph‐American Geophysical Union. Vol.167 p.283.

4. F2-layer height of the peak electron density (hmF2) dataset employed in Inferring Vertical Plasma Drift – Data of Best fit

5. Daily, seasonal and monthly variation of middle‐low latitudes magnetic field during low solar activity;Adhikari B.;Discovery,2017

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