and 2.13 billion Philippine Pesos (1987 pesos) in damage, or US$103.6 million (1987 dollars). Severe Tropical Storm Ellis The initial disturbance formed west of Kosrae on October 13, moving west-northwest. Slow to organize, the system evolved into a tropical depression on October 16 and a tropical storm late that day. Soon afterwards, Ellis turned westward and slowed due to a weakness in the subtropical ridge to its north caused by a system passing well to the north of Ellis. The storm turned southwest on October 17 due to the building in of a stronger high pressure system to its northwest. By October 20, Ellis weakened into a tropical depression while resuming a westward course as it passed under an upper-level low which increased vertical wind shear and disrupted its associated thunderstorm activity. The cyclone turned west-northwest on October 21 for a couple days before dissipating east of the Philippines. Typhoon Faye (Tasing) The initial tropical disturbance formed in the South China Sea, and was swept eastward through the Philippines due to Dot's movement to its north. The system emerged east of the Philippines and developed into a tropical depression and tropical storm on October 23. Turning northwest, Faye crossed central Luzon on October 24, weakening back into a tropical depression. Back in the South China sea, Faye regained tropical storm strength. The cyclone made a small cyclonic loop between October 25 and October 26 as a system over China approached Faye from the northwest. The tropical cyclone accelerated east-northwest, passing just north of Luzon. By October 28, Faye's motion slowed and the system strengthened into a typhoon early on October 29. After passing Okinawa, strong westerly winds aloft caused the typhoon to begin to weaken. Early on November 1, Faye weakened into a tropical storm before it evolved into an extratropical cyclone later that day. Tropical Storm Gordon The initial disturbance formed in the southern South China Sea and moved eastward. Its initial intensification to a tropical storm was caused by a surge in the northeast flow to its north and west, and the system turned to the north. As the cyclone became warm core, Gordon was able to restrengthen into a tropical storm after the monsoon wind surge slackened. Throughout its life cycle, thunderstorm activity was removed to the northwest of Gordon's low level circulation. Soon after becoming a tropical storm again, Gordon turned to the west-northwest and made