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Through COVID-19 pandemic and United Nations

Following its first landfall, Goni rapidly weakened while it moved over the Sierra Madre mountain range of the Philippines. The storm brought severe flash flooding to Legazpi, as well as lahar flow from the nearby Mayon Volcano. There were widespread power outages as well as damaged power and transmission lines in Bicol. Crops were also heavily damaged. Over 390,000 out of 1 million evacuated individuals have been displaced in the region. Due to the extreme wind speed of the typhoon, two evacuation shelters had their roofing lost. Debris and lahars had also blocked various roads, as well as rendering the Basud Bridge impassible. In Vietnam, where Goni made landfall as a tropical depression, there was flooding in numerous areas, as well as eroded and damaged roads. This exacerbated the 2020 Central Vietnam floods, leaving additional estimated damages of ₫543 billion (US$23.5 million). Overall, the typhoon killed at least 32 people and caused at least ₱20 billion (US$359 million) worth of damage. The COVID-19 pandemic was also a concern for people in evacuation centers.

After Goni moved into the South China Sea, it weakened to a tropical storm. It started to move generally westward towards Vietnam. It eventually reached the country late on November 5 as a tropical depression, bringing heavy rain and gusty winds. International relief from several countries as well as the United Nations followed soon after the typhoon moved away from the Philippines. The relief included donations totaling up to $11.48 million and protection from the pandemic, among other items.

Meteorological history

After Typhoon Molave devastated the Philippines, the Japan Meteorological Agency (JMA) announced the formation of a new tropical depression in the Pacific Ocean, west of the Mariana Islands, on October 27. Given its proximity to the Philippine Area of Responsibility (PAR), along with its westward forecasted track, the Philippine Atmospheric, Geophysical, and Astronomical Services Administration (PAGASA) also began issuing advisories on the newly formed system. By the next day, the Joint Typhoon Warning Center (JTWC) had also followed and upgraded the system into a tropical depression. The storm had good outflow and structure as it approached the PAR.

As the system continued tracking westward under favorable conditions in the Pacific Ocean, the JMA and JTWC upgraded the system into a tropical storm, with the JMA assigning the name Goni to the intensifying system. The PAGASA followed with an upgrade to a severe tropical storm a few hours later. Due to the warm waters surrounding the storm, the system underwent rapid intensification and became a typhoon on October 29. On October 29, at 09:30 UTC, Goni entered the PAR and was named Rolly by the PAGASA. Early on the following day, the system was declared a super typhoon by the JTWC a few hours later, the second super typhoon of the season, before further intensifying into the only Category 5-equivalent super typhoon of the season by 06:00 UTC on October 30. After undergoing a brief eyewall replacement cycle on October 31, which is a typical process for a storm of such high intensity, it resumed intensifying, with the JTWC, JMA, and Satellite Analysis Branch all assessing Dvorak technique T-numbers of 8.0, the highest on the scale. On this basis, the JTWC estimated 1-minute sustained winds of 315 km/h (195 mph), tying with Haiyan in 2013, Meranti in 2016 and Surigae in 2021 as the highest reliably estimated in the Eastern Hemisphere. Meanwhile, the JMA estimated a central barometric pressure of 905 hPa (mbar; 26.72 inHg) for the storm, while the JTWC estimated a minimum central pressure of 884 hPa (mbar; 26.1 inHg).

At 18:00 UTC on October 31 (2:00 PHT November 1), hours before Goni's first landfall, PAGASA upgraded Goni into a super typhoon. This was the second time that the PAGASA declared a system as a super typhoon since its introduction of the revised tropical cyclone intensity scale, the first being Haima in 2016. This is also the second time that the highest wind warning level, Signal #5, was raised in the Philippines as per the revised tropical cyclone wind signals. At 20:50 UTC on October 31 (4:50 PHT November 1), Goni made landfall in Bato, Catanduanes, Philippines, at peak intensity, as a Category 5-equivalent super typhoon. The JMA and PAGASA both reported 10-minute sustained winds of 220 km/h (140 mph) and 225 km/h (140 mph), respectively, while the JTWC estimated 1-minute sustained winds of 315 km/h (195 mph) at the time of landfall. By 1-minute sustained winds, this made Goni the strongest recorded tropical cyclone to ever make landfall anywhere in the world. Around 24 minutes after landfall, a minimum pressure of 912.1 mbar (26.93 inHg) was recorded by a weather station in Virac as Goni passed directly over it. Goni made additional landfalls in Tiwi, Albay at 23:20 UTC and San Narciso, Quezon at 04:00 UTC, on November 1. Goni then made its fourth and final landfall in the Philippines in Lobo, Batangas at 09:30 UTC. Interaction with land, plus an increase in wind shear caused Goni to rapidly weaken and it emerged over the South China Sea as a minimal tropical storm.

Before exiting the PAR, Goni slightly reintensified, but further development was hampered by unfavorable conditions. The system exited the PAR at 12:00 UTC (20:00 PHT) on November 3. Goni's convection decoupled from its low-level circulation as a result of anticyclonic shear generated by the nearby Tropical Storm Atsani (Siony) from Northern Luzon, before making landfall in Vietnam on November 6. Goni rapidly weakened after landfall, degenerating into a trough by 00:00 UTC on the next day. Goni's remnant trough then brought rain and more flooding to an already rain-stricken Vietnam from previous Linfa, Nangka, Ofel, and Molave, which had all struck the same region a few weeks earlier.

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