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This manuscript presents the first observation of the interaction between a brightness wave (BW) associated with the midnight temperature maximum (MTM) and equatorial spread F (ESF) airglow depletions. The study indicates that as the BW passes through the ESF depletion, the depletion evolves into an enhancement in one hemisphere, attributed to neutral winds related to the MTM/BW. Data from all-sky imagers in South America were utilized to analyze this phenomenon, highlighting the complex dynamics of the low

Author

betetof140

Language

EN