SWIO
editOn September 24, the MFR noted that tropical cyclogenesis would be possible in late September due to the passage of an equatorial Rossby wave and an Kelvin wave, which would help cause the formation of a temporary near-equatorial trough.[1] The next day, a near-equatorial trough would begin forming, of 65°E, featuring moderate convective activity on its polar side.[2]
References
edit- ^ Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean (PDF) (Report). Météo-France. 24 September 2024. Retrieved 27 September 2024.
- ^ Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean (PDF) (Report). Météo-France. 25 September 2024. Retrieved 27 September 2024.