source: Early September 12, dry air wrapping around the southern area of the cyclone caused most of the heat to leave.
target: Dry air wrapping around the southern edge of the cyclone eroded most of the deep convection by early September 12.
references: Dry air wrapping around the southern edge of the cyclone eroded most of the deep convection by early September 12. Dry air wrapping around the southernmost part of the cyclone caused a reduction in the storm's upward mobility by early on September 12. Dry air wrapping around the southern periphery of the cyclone eroded most of the deep convection by early on September 12. Dry air wrapping around the southern periphery of the cyclone eroded the deep convection by September 12. Dry air surrounding around the southern periphery of the cyclone destroyed most of the deep displacement by early on September 12. Most of the deep convection of the cyclone eroded . This was due to dry air covering around the southern peripher of the cyclone . This was on early 12 September. Dry air protect around the southern periphery of the cyclone eroded most of the deep convection by early on September 12.