Typhoon Yunya, known in the Philippines as Typhoon Diding, was a strong tropical cyclone whose landfall in the Philippines coincided with the 1991 eruption of Mount Pinatubo. A small tropical cyclone, Yunya rapidly developed from a tropical disturbance near East Samar on June 11. By June 13 the storm had reached typhoon status as it moved west-northwest near the Philippines. Yunya attained its peak intensity the following day with estimated winds of ; however, strong wind shear soon impacted the typhoon and caused it to rapidly decay. The storm struck southern Luzon early on June 15 as a minimal typhoon before moving over the South China Sea later that day. After turning north and weakening to a tropical depression, the system brushed the southern tip of Taiwan on June 16 before dissipating the following day.
Across the Philippines, Yunya produced heavy rains that triggered significant flooding. Hundreds of homes and several bridges were washed away by swollen rivers. Six people were killed as a direct result of the storm, 2,013 homes were destroyed, and 24 others were damaged. Although the storm itself caused significant damage, the worst effects were related to the system's heavy rains mixing with volcanic ash from Mount Pinatubo, creating massive lahars that killed 320 people.
Meteorological history
On June 11, 1991, a tropical disturbance developed east of East Samar. Situated to the southwest of a tropical upper tropospheric trough, the system experienced low wind shear and gradually intensified as it moved northwestward. The following day, the Japan Meteorological Agency (JMA) began monitoring the system as a tropical depression. At 15:00 UTC on June 12, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert on the depression. Around this time, the storm began a period rapid development and a tiny central dense overcast formed. At 18:15 UTC, the USNS Spica sailed directly through the storm, measuring a barometric pressure of 989.5 mbar (hPa; 29.22 inHg) and peak winds of . Although Yunya was already a tropical storm, the JTWC did not issue their first advisory on the system until early on June 13, at which time they assigned it the name Yunya. Throughout June 13, subsidence around the periphery of Yunya allowed the system to develop good outflow. As a result, the storm attained typhoon status later that day before strengthening slowed. By June 14, Yunya turned towards the west-northwest in response to a subtropical ridge to the north. Following this turn, the typhoon attained its peak intensity as a Category 3-equivalent typhoon on the Saffir–Simpson scale with winds estimated at .
thumb|right|Satellite image of Yunya as it made landfall; the [[eruption column from Mount Pinatubo (in dark grey) can clearly be seen through the storm's clouds]]
Within hours of reaching its peak strength on June 14, strong wind shear associated with a second subtropical ridge over Asia impacted the typhoon. Due to the system's small size, the shear was able to disrupt the cyclone's core and cause rapid weakening as it approached southern Luzon. Around 00:00 UTC on June 15, Yunya made landfall just north of Dingalan Bay as a minimal typhoon and weakened to a tropical storm shortly thereafter. As the storm moved across Luzon, Mount Pinatubo, a volcano in the Zambales Mountains on the island's western side, was experiencing a major eruption—the second-largest to occur during the 20th century. Due to Yunya's circulation, the massive cloud of ash produced by the eruption was moistened and redistributed over the Philippines instead of blowing out to sea, greatly exacerbating the impact of the event. By June 15, air-borne ash combined with the typhoon's rainfall, resulting in widespread travel disruptions and structural collapses. The mixture also made it appear as through it was nighttime during the middle of the day, prompting concern from residents. which prompted most of the airports in the country to close and Philippine Airlines to cancel all domestic and international flights through June 19. Low to mid-level winds and heavy rains from the storm contributed to widespread tephra falling over an area of of central and western Luzon. Heavy rains also resulted in lahars along mountains between the Gumain River to the Sacobia River and between Sacobia River to the O'Donnell River. These lahars inundated crops and homes, especially along the Abacan River. As a result of the lahars, some buildings and all bridges in Angeles City were destroyed. Moreover, 320 people were killed and 279 others were injured. The United States Geological Survey believes that the death toll from the lahars would have been far lower if not for Yunya. and one person was killed after the roof of a bus terminal collapsed under the weight of ash and rain. Two people died and three others were injured in an accident near Clark Air Base, Along the Sacobia River in Pampanga, at least 170 homes were washed away due to the storm. The Abacan bridge spanning the Abacan River collapsed with a truck carrying three people, and an empty car. It is unknown whether the three people survived. Civil defense officials confirmed that five other bridges collapsed in Pampanga and Zambales provinces. All crops were destroyed throughout Iriga. Overall, 2,013 homes were destroyed and 24 others were damaged during the passage of the typhoon. A total of 2,035 families or 10,185 people were evacuated to shelters. Excluding from lahars, six people were killed by Yunya.