for further development, with warm sea surface temperatures and low wind shear. At 00:00 UTC on June 11, the JMA upgraded the system into a tropical depression. Six hours later, the JTWC issued a TCFA for the system as it began to show characteristics of a monsoon depression. By 18:00 UTC, the JMA upgraded the system to a tropical storm, assigning it the name Koguma. On June 12 at 00:00 UTC, the JTWC upgraded Koguma to a tropical depression, assigning it the designation 05W. Later that day, the JTWC also upgraded Koguma to a tropical storm. By June 12, it had made landfall southeast of Hanoi, dissipating on the next day. 1 person died in Yên Bái province as a result of Koguma. Typhoon Champi At 00:00 UTC on June 18, the JTWC started to monitor a broad area of convection nearly to the south-southwest of Pohnpei. The system remained weak as it moved northwestwards in a favorable environment for further intensification, characterized by warm sea surface temperatures, low to moderate wind shear and good outflow; the disturbance remained weak as it moved northwestwards. The JTWC issued a TCFA on the system two days later, though the system remained disorganised. The JMA upgraded the system to a tropical depression at 00:00 UTC on June 21. Meanwhile, the JTWC designated it as 06W in their first advisory on the system, with an exposed LLCC being evident on satellite imagery due to moderate wind shear, being induced by a tropical upper tropospheric trough to its north. By 21:00 on June 21, 06W made its closest passage to the south-southwest of Guam, continuing its northwest track. On June 22, at 06:00 UTC, the JTWC upgraded the system into a tropical storm as it continued to move away from Guam. The JMA followed and upgraded the system into a tropical storm, in June 23 at 00:00 UTC, and assigned it the name Champi. At 18:00 UTC, the JMA upgraded the storm to a severe tropical storm as it turned northwestwards. At this time, a microwave imagery scan of Champi revealed an eye feature emerging in the system; however, this was short lived as dry air continued to impact the storm from the west. In addition, poleward outflow on the system remained weak on June 24, restricting Champi to significantly develop. However, on the next day, as a shortwave trough crossed the Ryukyu Islands, the