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On October 27, 1997 the Fiji Meteorological Service's Regional Specialized Meteorological Center in Nadi, Fiji (RSMC Nadi) started to monitor a weak tropical disturbance that had developed to the north of the Northern Cook Islands.
Initially a tropical disturbance between Kosrae and Enewetak on November 6, the system moved south of west until November 9, when the system began tracking north of west.
During January 2, RSMC Nadi reported that Tropical Disturbance 07F had developed to the southeast of Futuna Island.
On January 12, a tropical disturbance formed in the Coral Sea.
During January 2, 2014 the Fiji Meteorological Service's Regional Specialized Meteorological Center in Nadi, Fiji (RSMC Nadi) reported that Tropical Disturbance 07F had developed to the southeast of Futuna Island.
On December 23, the Joint Typhoon Warning Center (JTWC) reported that a tropical disturbance had developed within the monsoon trough about 1540 km (960 mi) to the east of Medan in Indonesia.
The origin of Typhoon Durian can be traced to a tropical disturbance that developed near Chuuk State in the Federated States of Micronesia on November 23.
Typhoon Durian's meteorological history began with its origins as a tropical disturbance near Chuuk State and lasted until its dissipation off the coast of Andhra Pradesh, India.