The tropical cyclone named Clarence originated in the southern Indian Ocean. It formed in the region near the Western Australia coastline and moved eastwards towards the open waters of the Indian Ocean.
Tropical cyclones, also known as hurricanes or typhoons depending on the region, typically form over warm ocean waters near the equator. Clarence, specifically, originated in the southern Indian Ocean. This area is known for being prone to cyclone activity, especially during the cyclone season. The warm ocean waters in the region provide the necessary energy and moisture for the development and intensification of tropical cyclones. As Clarence formed, it moved eastwards away from the coast and into the open waters of the Indian Ocean, potentially impacting nearby islands or coastal regions depending on its trajectory and intensity.