At 0600 UTC (11 a.m. PST) on June 28, the Pakistan Meteorological Department (PMD) issued its first advisory regarding the remnants of the system. The PMD stated that the remnants had the potential to cause widespread heavy rain with strong winds in Sindh, Balochistan, Azad Kashmir and North-West Frontier provinces. This could worsen conditions in areas already flooded by Tropical Cyclone Yemyin. In its fourth advisory on July 1, the PMD warned about the high probability of the system moving westward towards southern Sindh (instead of northwestward as previously projected), and regenerating over the Arabian Sea. The remnants of Tropical Cyclone 04B were mentioned in a Significant Tropical Weather Advisory from the JTWC early on July 2. After crossing the Deccan Plateau, convection was southwest of the centre, in the Arabian Sea, while multiple associated low-level circulation centres had yet to re-emerge, and were located in west-central India, north-northeast of Mumbai. The area had favourable upper-level divergence, but high vertical wind shear. Eventually, the circulation centre became fully exposed in unfavourable conditions, and the JTWC declared it no longer suspect for development later that day.