When there are trade winds of course the effect disappears, but afterwards, as soon as the wind stabilizes, you see again that the rainfall peaks come back above this area.
Ketika ada angin musiman tentu saja efek tersebut menghilang, tapi setelah itu, begitu anginnya stabil kembali, Anda lihat lagi bahwa puncak curah hujan kembali ke atas area ini.