An area of thunderstorms developed in the Mozambique Channel on January 25,2004, about 95 km (60 mi) west of Madagascar, the convection persisted around a mid- to low-level circulation.
An area of thunderstorms developed in the Mozambique Channel on January 25,2004, about 95 km (60 mi) west of Madagascar. Located within an area of moderate wind shear, the convection persisted around a mid- to low-level circulation.