Tsunamis in 2018

September 4, 2018 Tsunami: Southern Japan

September 4, 2018 · 1.29 m · Deaths: few · Definite tsunami

A tsunami of meteorological origin began at Southern Japan on September 4, 2018. The water rose as high as 1.29 meters. Its effects were recorded at 8 places.

Where the waves reached

The source (white) and every runup with a place, colored by the water height recorded there. A ring is a runup NCEI marks doubtful.

  • Under 1 m
  • 1 to 3 m
  • 3 to 10 m
  • 10 to 30 m
  • 30 m and more
  • Height not recorded

Tsunami warnings in force

The tsunami

Date
September 4, 2018
Source
Southern Japan
Cause
Meteorological
Maximum water height
1.29 m (4.2 ft)
Runups recorded
8
Waters
Ocean
How certain
Definite tsunami

The toll

Deaths
Few (about 1 to 50) with the earthquake or eruption that caused it
Damage
Limited (under about $1 million); Extreme (about $25 million or more) with the earthquake or eruption that caused it

Where the literature gives no number, NCEI records a description on a scale of 1 to 4, printed here in its words. Damage is in millions of US dollars of the year of the event, not adjusted for inflation.

What the record says

NCEI’s account, from the sources it cites.

Reference #14273:

Typhoon Jebi was the most powerful typhoon to strike Japan in 25 years. It was formed as a tropical depression on 26 August 2018 and then rapidly intensified into a typhoon. This typhoon destructively affected the Northern Mariana Islands and then on 2 September caused huge waves and five fatalities on the coast of Taiwan. Propagating north-westward and then northward on 4 September, Jebi reached the south-eastern coast of Japan producing severe damage and intensive floods along the entire coasts of Shikoku Island and the Kansai region of Honshu Island. The typhoon existed for 15 days and ended on 9 September 2018.

The entire character of seiche generation by the propagating 2018 typhoon was comparable to that for the 2016 typhoon Lionrock. Similar to the 2016 event, the broad-band oscillations decay quickly after the 2018 typhoon’s passage, while narrow-band oscillations at resonant frequencies keep reverberating. In general, we may conclude that local topography (eigen properties of specific harbours and bays) plays a critical role in the generation of the extreme seiches, which can be considered as meteotsunamis. In this regard, these conclusions are in good agreement with those by Honda et al. (1908) and Nomitsu (1935), who were the first to show that the resonant properties of specific sites are central to the formation of tsunamis and tsunami-like waves on the coast of Japan.

Every runup

Nearest the source first. Heights are above sea level at the time; a tide gauge reads half the wave’s full height.

WhereCountryKm from sourceWater height, mInland, mMeasured byFirst wave, UTCDeaths
TannowaJapan0.35Tide gauge (half the maximum wave height)
YukiJapan0.69Tide gauge (half the maximum wave height)
SumotoJapan0.4Tide gauge (half the maximum wave height)
KomatsushimaJapan0.41Tide gauge (half the maximum wave height)
KushimotoJapan0.69Tide gauge (half the maximum wave height)
GoboJapan1.29Tide gauge (half the maximum wave height)
MurotomisakiJapan0.64Tide gauge (half the maximum wave height)
Tosa-ShimizuJapan0.44Tide gauge (half the maximum wave height)

More

Every tsunami in 2018The 2000sTsunamis of JapanThis day in weather historyAlerts in force

Sources

Tsunami events and runups from NOAA’s National Centers for Environmental Information, Global Historical Hazard Database, cited as NCEI/WDS, doi:10.7289/V5PN93H7. Public domain. Read 2026-09-24. NCEI tsunami event 6114.