D‐region ionosphere response to the total solar eclipse of 22 July 2009 deduced from ELF‐VLF tweek observations in the Indian sector

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dc.contributor.author Singh, Rajesh
dc.contributor.author Veenadhari, B.
dc.contributor.author Maurya, A.K.
dc.contributor.author Cohen, Morris B.
dc.contributor.author Kumar, Sushil
dc.contributor.author Selvakumaran, R.
dc.contributor.author Pant, P.
dc.contributor.author Singh, Abhay K.
dc.contributor.author Inan, Umran S.
dc.date.accessioned 2015-10-19T07:39:48Z
dc.date.accessioned 2021-02-12T09:21:08Z
dc.date.available 2015-10-19T07:39:48Z
dc.date.available 2021-02-12T09:21:08Z
dc.date.issued 2011
dc.identifier.citation JGR, 116, A10301, doi:10.1029/2011JA016641, 2011 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/625
dc.description.abstract Observations of tweeks with higher harmonics (n > 1) at low latitude stations Allahabad and Nainital, in the Indian sector, during the total solar eclipse on 22 July 2009, are presented. Allahabad and Nainital stations were in 100% and 85% of the totality paths. Observations suggest that about 30–40% obscuration of solar disc can lead to the tweeks occurrence which otherwise occur only in nighttime. A total of 148 tweeks at Allahabad and 20 tweeks at Nainital were recorded with some of them up to 3rd harmonics. The World Wide Lightning Location Network data indicated that tweeks observed were generated by lightning’s located in the partial eclipse area of Asia‐Oceania region. The changes in D‐region ionospheric VLF reflection height and electron density (∼22–23 cm−3) during eclipse have been estimated from the first cut‐off frequency of the tweeks. The reflection height increased from ∼89 km from the first occurrence of tweek to about 91–92 km at the totality and then decreased to ∼87 km at the end of the eclipse, suggesting a change of about 5 km in the reflection height during eclipse. The reflection heights are lower by 2–3 km as compared to normal nighttime tweek reflection heights. The above increase in the reflection height indicate that the partial nighttime condition is created during eclipse, as the main D‐region ionizing radiation Lyman a is blocked but solar soft X‐ray and EUV radiations originating from the limb solar corona are not totally blocked which produce some of ionization in the D‐region. en_US
dc.language.iso en en_US
dc.subject D-region ionosphere en_US
dc.subject Solar eclipse en_US
dc.subject ELF en_US
dc.subject VLF en_US
dc.subject Tweeks en_US
dc.subject Allahabad en_US
dc.subject Nainital en_US
dc.subject Solar radiation variations en_US
dc.title D‐region ionosphere response to the total solar eclipse of 22 July 2009 deduced from ELF‐VLF tweek observations in the Indian sector en_US
dc.type Article en_US
dc.identifier.accession 091179


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