A total of 16 houses were destroyed during the storm (totally or partially), 40 hectares of palay to tillering stage and 15 hectares in ripening stage were damaged on some parts of Iloilo, and a total of ₱1,500,000 (US$28,788) as reported damages to infrastructure. In response, the DSWD provided a total of ₱24,9049.57 ($47,79.58 USD) to the affected families on Surigao del Norte and Surigao del Sur. Nock-ten was first noted as a tropical depression on December 21, and quickly organized into a tropical storm. The system reached severe tropical storm intensity the following day, and then typhoon intensity the day after. Around this time, a well-defined eye formed, and the storm began rapidly intensifying. Nock-ten reached its peak intensity as a Category 5-equivalent super typhoon with 1-minute sustained winds of 260 km/h (160 mph) on December 25, becoming the strongest tropical cyclone recorded on Christmas Day anywhere in the world since at least 1960 in terms of 1-minute sustained winds. Shortly thereafter, land interaction imparted weakening, with warming cloud tops, and the typhoon made its first landfall over Catanduanes as a Category 4-equivalent super typhoon with 1-minute sustained winds of 250 km/h (155 mph). Nock-ten emerged into the South China Sea as a minimal typhoon, where strong vertical wind shear associated with a cold surge event led to continued weakening, with the low-level circulation center becoming exposed. The JMA issued its final advisory on the system late on December 27, and the JTWC followed suit early on December 28. On June 23, the JMA started to monitor a broad tropical depression that had developed, about to the southwest of Manila in the Philippines. The system was located within a favourable environment for further development, but was not expected to significantly develop any further, as an upper level low was expected to move over the system. Over the next couple of days the system moved north-westwards, before the system dissipated and became a remnant area of low pressure during June 25. However, the system's remnants were tracked until they made landfall on central Vietnam during June 27. The system was responsible for some heavy rainfall in Central and Southern Vietnam. The JMA upgraded a low-pressure area east of Taiwan to a tropical depression on August 6.