| Texto completo | |
| Autor(es): |
Sousasantos, Jonas
[1]
;
Andrade Sobral, Jose Humberto
[1]
;
Kherani, Esfhan Alam
[1]
;
Fares Saba, Marcelo Magalhaes
[1]
;
de Campos, Diovane Rodolfo
[1]
Número total de Autores: 5
|
| Afiliação do(s) autor(es): | [1] Inst Nacl Pesquisas Espaciais, BR-12227010 Sao Jose Dos Campos, SP - Brazil
Número total de Afiliações: 1
|
| Tipo de documento: | Artigo Científico |
| Fonte: | Annales Geophysicae; v. 36, n. 2, p. 349-360, MAR 9 2018. |
| Citações Web of Science: | 0 |
| Resumo | |
The vertical coupling between the troposphere and the ionosphere presents some remarkable features. Under intense tropospheric convection, gravity waves may be generated, and once they reach the ionosphere, these waves may seed instabilities and spread F and equatorial plasma bubble events may take place. Additionally, there is a close association between severe tropospheric convection and lightning strikes. In this work an investigation covering an equinox period (September-October) during the deep solar minimum (2009) presents the relation between lightning strike activity and spread F (equatorial plasma bubble) detected over a low-latitude Brazilian region. The results show a considerable correlation between these two phenomena. The common element in the center of this conformity seems to be the gravity waves. Once gravity waves and lightning strikes share the same source (intense tropospheric convection) and the effects of such gravity waves in the ionosphere include the seeding of instabilities according to the gravity waves magnitude, the monitoring of the lightning strike activity seems to offer some information about the subsequent development of spread F over the equatorial region. (AU) | |
| Processo FAPESP: | 12/15375-7 - Características dos raios ascendentes no Brasil |
| Beneficiário: | Marcelo Magalhães Fares Saba |
| Modalidade de apoio: | Auxílio à Pesquisa - Regular |