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AIRS data on April second at 05:41 UTC showed a cluster of strong thunderstorms surrounding the weak center of circulation of TD1W. Some of those thunderstorms were dropping heavy rainfall and had very high cloud tops, so high they were as cold as -63 Fahrenheit/-52 Celsius. On April 2, TD1W was located about 280 miles east-southeast of Ho Chi Minh, Vietnam near 9.3 North latitude and 111.2 East longitude. It was moving very slowly at 1 knot to the west and maximum sustained winds were near 25 knots. By April 3 at 0900 UTC it had continued moving slowly, only at a rate of 2 knots westward and was then 315 miles (506 km) east-southeast of Ho Chi Minh, Vietnam near 9.1 North and 111.7 East. It still had maximum sustained winds near 25 knots, but wind shear was battering the system.
On April 4 NASA's Aqua satellite passed overhead once again and noticed that TD1W had become much more disorganized and spread out. By the fourth, TD1W had also moved more than 45 miles farther away from Vietnam and into the South China Sea. Strong convection appeared scattered and disorganized on AIRS' infrared imagery and not around the center of circulation.
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