Hudhud
Crossed the Andaman Islands, intensified across the Bay of Bengal and came ashore directly over Visakhapatnam on 12 October, where it tore the roof off the airport terminal and closed VTZ for days.
NOAA IBTrACS dataset ↗Plan around the weather
See where tropical cyclones have historically travelled—and compare the months when weather disruption is most likely to affect your trip.
Every line is plotted from six-hourly latitude and longitude records in NOAA IBTrACS. Click a line to identify the storm and route.
Observed tracks: Actual six-hourly positions selected from NOAA IBTrACS v04r01, not forecasts or illustrative paths. Start and endpoint markers are outlined; peak intensity is solid. Basemap © OpenStreetMap contributors.
Pabuk gives Thailand a direct example; rare near-equatorial Vamei gives the Singapore–Malaysia area one. Each mini-trail uses exactly the same coordinates as the map.
Crossed the Andaman Islands, intensified across the Bay of Bengal and came ashore directly over Visakhapatnam on 12 October, where it tore the roof off the airport terminal and closed VTZ for days.
NOAA IBTrACS dataset ↗Came ashore at Gopalpur on 12 October at the height of the post-monsoon season. Around a million people were moved off the coast beforehand, and the death toll stayed in the dozens where the same coast had lost thousands in 1999.
NOAA IBTrACS dataset ↗Ashore near Puri on 3 May, and rare for it: the Bay of Bengal's severe storms almost all come after the monsoon, not before. It spent nine days over water building strength and closed Bhubaneswar on the way through.
NOAA IBTrACS dataset ↗Yolanda
Crossed the central Philippines before continuing through the South China Sea into Vietnam and southern China.
NOAA IBTrACS dataset ↗Ompong
Crossed northern Luzon, passed south of Hong Kong and made landfall on the Guangdong coast.
NOAA IBTrACS dataset ↗Isang
Crossed the Luzon Strait and intensified before landfall near Macao and Zhuhai.
NOAA IBTrACS dataset ↗Egay
Passed north of Luzon, crossed the Taiwan Strait and tracked inland after landfall in Fujian.
NOAA IBTrACS dataset ↗Crossed the Gulf of Thailand and made landfall in Nakhon Si Thammarat before moving into the Andaman Sea.
NOAA IBTrACS dataset ↗Formed about 130 km east of Singapore, passed just north of the city and crossed southern Peninsular Malaysia.
NOAA IBTrACS dataset ↗Country comparison
Higher bars mean greater historical travel-disruption exposure—not a prediction that a storm will occur during your trip.
MNL · CEB
Around twenty storms enter Philippine waters a year and eight or nine come ashore. Where matters as much as when: Cagayan Valley, Bicol and Eastern Visayas take most of them, while Palawan and the western Visayas are hit far less. The tracks also shift south as the season runs on, so mid-year is worst in the north and the later months worst for the central islands. From Wind Signal No. 3 the airports under it generally stop.
MAA · CCU · VTZ · BBI
Two seasons rather than one: a smaller peak before the monsoon in May, and the real one through October and November. Fewer storms form here than in the Pacific, but the Bay of Bengal is shallow and funnel-shaped, so it is the surge they push ashore that closes the coast. Andhra Pradesh and Odisha take most of the landfalls; the Arabian Sea side at Mumbai and Goa is far quieter.
PVG · SHA · CAN
Guangdong and Fujian take most of the landfalls, but Shanghai loses more flights to storms that never arrive — a track running north up the coast is enough to empty Pudong without making landfall at all.
BKK · HKT
The two coasts have opposite bad seasons: Phuket and the Andaman side are wettest from May to October, the Gulf and Samui from November into December. Storms usually cross Vietnam first and arrive overland already weakened, so what closes a runway here is rain and thunderstorms rather than wind.
SIN
Barely a degree off the equator, which is too close for a cyclone to spin up at all — Vamei in 2001 is the only one on record anywhere near here, and it is in the archive on the main page. What delays flights is the afternoon convection of the two monsoons, and storms elsewhere in the region arriving as knock-on delays.
TPE · KHH
The central range rises to nearly four thousand metres and pulls storms apart as they cross, which shelters the western plain where Taoyuan sits. It does that by wringing the rain out of them, so the disruption is as often flooding and closed ground transport as wind at the airport itself.
OKA · KIX · HND
Okinawa and the Ryukyus are in the path from June and take several close passes a year. Honshu's season is shorter and later — August into September — and a storm that gets that far north has usually weakened or begun turning extratropical, which widens its wind field rather than shrinking it. Tokyo loses flights to storms that never come near it.
ICN · PUS · CJU
A short, sharp season: almost nothing before August, then a few concentrated weeks. Storms reaching this far north are recurving and moving fast, which limits how long they sit over any one place but not how hard they blow. Jeju is on the recurve path and usually the first thing hit; Busan and the south coast far more often than Seoul.
HKG
Only two direct strikes since 1987, but the flight-stopping storm signal is raised almost every year.
DAD · HUI · HAN
Storms land between Hue and Da Nang far more than anywhere else; Ho Chi Minh City in the south is rarely affected.
GUM · SPN
The only entry here with no real off-season — a typhoon can strike within three days at any time of year.
A different kind of risk
Indonesia sits close enough to the equator that it is rarely reached by a named tropical cyclone at all. Its real aviation risk is volcanic ash: several volcanoes carry active advisories most of the year, and that risk does not run on a season the way a typhoon does.
Jakarta–Denpasar flights already fly directly through SEMERU's current ash advisory.
Not seasonal: an ash advisory is issued when a volcano is erupting, not on a calendar, so there is no month-by-month chart to draw for it. View live volcanic ash advisories →