was known as Loleng. Typhoon Walt (Miding) Walt was part of a three tropical cyclone outbreak along a reverse-oriented monsoon trough (aligned northeast–southwest rather than the usual northwest–southeast orientation.) By July 11, a thunderstorm cluster developed near Palau. The disturbance moved slowly northwest, becoming a tropical depression late on July 14. As it neared the 15th parallel, Walt turned to the northeast and intensified. By the afternoon of July 19 the cyclone had become a super typhoon, the first of the season, an intensity it maintained for a day. While slowly weakening, Walt turned to the west. By the morning of July 23 the cyclone had dropped down to tropical storm strength as it turned to the north for a couple days. The storm turned back to the west, making landfall on the southwest end of Shikoku as a moderate tropical storm, bringing wind gusts to tropical storm force. The cyclone dissipated south of Korea by early on July 27. Rainfall across South Korea helped improve severe drought conditions. Tropical Storm Yunya (Norming) The disturbance that was to become Tropical Storm Yunya was first mentioned on July 16 by the Joint Typhoon Warning Center when it was located in the South China Sea as cloudiness in a reverse-oriented monsoon trough. A weak low-level circulation was identified through animated satellite imagery and synoptic data early that morning. Moving east-northeast, the system strengthened into Tropical Depression 11W by July 18. At 0600 UTC that day, the Japan Meteorological Agency declared the formation of Tropical Storm Yunya. Yunya continued to undergo gradual strengthening, reaching its peak strength near landfall in northwest Luzon on the morning of July 19. As it tracked over land, it became disorganized and weakened to a minimal tropical storm. In the Philippine Sea, Yunya briefly restrengthened and reached a secondary peak of . The JMA discontinued warnings after it deemed Yunya to have dropped below tropical storm intensity at 1800 UTC that day, while the JTWC continued monitoring the tropical depression until convection decreased and the storm dissipated on July 21. During its life, Yunya had an unusual eastward motion, which was due to the reverse-oriented monsoon trough. Yunya was also a small system, and appeared to have been undergoing a period of rapid organisation of convection shortly before it made landfall. Heavy rain from Yunya caused landslides of volcanic debris from Mount Pinatubo. Coincidentally, a previous Typhoon Yunya