its peak wind spreed, with winds of respectively. Typhoon Freda began to round the western periphery of a ridge, which caused the system to accelerate towards the north. The JTWC estimated that Freda weakened to a tropical storm during the evening hours of September 13; however, the JMA maintained the storm at typhoon intensity for several additional days. By September 16, Freda began to interact with a mid-level trough to the north, which resulted in a turn to the northeast. After bypassing Honshu, wind shear began to take toll on the system and Freda began to turn extratropical. On September 17, the JTWC declared Freda extratropical, with the JMA doing the same the following day. It was lasted noted on September 20. Due to the storms erratic motion during its early stages, Guam received two distinct periods of heavy rainfall from the storm. On September 4, the typhoon dropped , and four days later, was recorded on the island, along with gale-force winds. Throughout the Mariana Islands, rough seas damaged coral reefs and eroded beaches, but there were no casualties. Typhoon Holly The final of a three storm tropical cyclone outbreak, Holly began as a poorly organized but persistent area of convection at the eastern edge of the monsoon trough, which was displaced a bit to the north of its climatological position. Tracking westward, the disturbance gradually organized due to low wind shear. Shower and thunderstorm activity developed over the center, and at 00:00 UTC on September 5, the JMA classified the system as a tropical depression, with the JTWC doing the same six hours later. Although only slight intensification was expected, the depression took advantage of the favorable conditions. A central dense overcast quickly developed, and the JMA upgraded Holly into a severe tropical storm at noon on September 7 and a typhoon 12 hours later. The JTWC also designated Holly a typhoon on September 7. Following a 36-hour period of rapid deepening, the JMA estimated that Holly attained its peak intensity of midday on September 9. Meanwhile, the JTWC estimated winds of , making Holly a super typhoon. Around this time, Holly veered from northwestward to northward caused by a weakness in the subtropical ridge. Holly steadily weakened as its forward motion decreased. On September 14, the JMA downgraded Holly to a severe tropical storm, while the JTWC estimated that Holly transitioned into a subtropical cyclone that day.