Daniel Bemmerer
(HZDR)
21/08/2025, 10:30
Giorgi Dalakishvili
(ISU)
21/08/2025, 11:00
Theoretically and by corresponding numerical simulations it is shown that the formation and localization of sporadic E (Es) layer at its mainly observable mid-latitude lower thermosphere heights can be determined by homogeneous horizontal wind velocity direction and value. In the suggested theory, differently from 'windshear' theory, the wind direction and value, in addition to geomagnetic...