March 19, 2017 Tsunami: Persian Gulf, Iran
A tsunami of meteorological origin began at Persian Gulf, Iran on March 19, 2017 at 04:30 UTC. The water rose as high as 3 meters. Its effects were recorded at 27 places in at least 3 countries. It killed 5 people.
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
The tsunami
- Date
- March 19, 2017, 04:30 UTC
- Source
- Persian Gulf, Iran
- Cause
- Meteorological
- Maximum water height
- 3 m (9.8 ft)
- Runups recorded
- 27
- Waters
- Ocean
- How certain
- Definite tsunami
- Source location
- 27.835° N, 51.940° E
The toll
- Deaths
- 5
- Injuries
- 22
- Damage
- $10 million
- Houses destroyed
- 85
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 #11764:
A second body was pulled from the coasts of Iran's southern port city of Dayyer on Monday evening, while four other victims are still unaccounted for after huge waves cause by a sea tornado -known as Seiche- pounded the coastal city on March 19, an official said. Speaking to Tasnim on Tuesday morning, Mohammad Hassan Basti, a deputy to governor of Iran's southern province of Bushehr, said the body of an eight-year-old boy was retrieved from the pier of Dayyer on Monday evening. He was the second victim among a total of six people lost in the deadly sea storm and subsequent flooding that hit Dayyer on Sunday, he noted. According to Basti, 22 people have been wounded in the incident, 80 dwellings have been destroyed, urban infrastructure has been damaged, and some 200 boats have been wrecked in the natural disaster. Head of Bushehr's Persian Gulf Oceanography Centre Ehsan Abedi had announced that the reason behind the giant waves and the sea overflow was a natural phenomenon called Seiche, saying it occurs when strong winds push water and cause water levels to drop at one end and rise at the other.
Reference #11970:
On 19 March 2017, a series of waves from the Persian Gulf inundated significant parts of the Port of Dayyer on the southern coastlines of Iran (Fig. 1), some time between 8:00 and 8:20 AM local time (4:30-4:50 GMT). It resulted in one death and five people missing, and reportedly capsized about 300 boats and caused ~$10 million of damage. According to Iranian state media, water progressed as far as ~1 km in land and video footage recorded by local individuals or seasonal travelers reveals surges of up to 2 m in a relatively calm, cloudy morning, even though a significant thunderstorm had occurred a few hours earlier. Local news outlets place the largest extent of destruction at Seyyed-Safa, a neighborhood close to the cruise port.
In summary, neither geological nor atmospheric sources can perfectly explain the distribution of amplitudes as obtained in our field survey. While we prefer the meteorological model, we suggest that its remaining misfits may be due to imprecisions in small-scale bathymetry and that future studies of the 19 March 2017 tsunami would warrant the use of a better bathymetry model for the region.
Reference #12474:
The waves affected about 40 km of the coastline, causing five deaths and injuring 20 people. Local authorities reported damage to ~300 fishing and recreational boats and 85 coastal properties.
The 2017 Dayyer event is the first known example of recorded destructive waves in the Persian Gulf, which caused severe damage and killed people.
Reference #12544:
The event was found to be very local; maximum trough-to-crest wave heights were 1.97 m at Dayyer and 2.34 m at Asaluyeh (both in Iran), near-field cities located * 80 km from each other; the dominant wave periods were 15-20 min. At all other sites, located along the entire coast of the Persian Gulf and in the Gulf of Oman, the observed wave heights were\35 cm.
Reference #13742:
During the 19 March 2017 event in the Persian Gulf, 5 people died and 22 people were injured
Every runup
Nearest the source first. Heights are above sea level at the time; a tide gauge reads half the wave’s full height.
| Where | Country | Km from source | Water height, m | Inland, m | Measured by | First wave, UTC | Deaths |
|---|---|---|---|---|---|---|---|
| Dayyer | Iran | 0 | Other | 2 | |||
| Dayyer (Municipal Jetty) | Iran | 0 | 2.5 | 170 | Runup height, post-tsunami survey | ||
| Dayyer (Coast) | Iran | 0 | 2.5 | 190 | Runup height, post-tsunami survey | ||
| Dayyer (Fishing Jetty) | Iran | 1 | 2.5 | 60 | Runup height, post-tsunami survey | ||
| Dayyer | Iran | 1 | 0.99 | Tide gauge (half the maximum wave height) | |||
| North Oli | Iran | 4 | 3 | 230 | Runup height, post-tsunami survey | ||
| Bardestan Estuary | Iran | 5 | 1 | 140 | Runup height, post-tsunami survey | ||
| Banak Park | Iran | 8 | 0.9 | 10 | Runup height, post-tsunami survey | ||
| Bibi-Khatoon | Iran | 13 | 2 | 600 | Runup height, post-tsunami survey | ||
| Demingez (II) | Iran | 21 | Runup height, post-tsunami survey | ||||
| Demingez (I) | Iran | 25 | 1.8 | 120 | Runup height, post-tsunami survey | ||
| Kali | Iran | 28 | 1.5 | 50 | Runup height, post-tsunami survey | ||
| Motaf Park (III) | Iran | 33 | 1.3 | Runup height, post-tsunami survey | |||
| Motaf Park (IV) | Iran | 33 | Runup height, post-tsunami survey | ||||
| Motaf Park (II) | Iran | 34 | Runup height, post-tsunami survey | ||||
| Motaf Park (I) | Iran | 35 | 0.3 | Runup height, post-tsunami survey | |||
| Asaluyeh | Iran | 78 | 1.17 | Tide gauge (half the maximum wave height) | |||
| Bushehr | Iran | 163 | 0.13 | Tide gauge (half the maximum wave height) | |||
| Ruwais | Qatar | 203 | 0.16 | Tide gauge (half the maximum wave height) | |||
| Doha | Qatar | 284 | 0.09 | Tide gauge (half the maximum wave height) | |||
| Dukhan | Qatar | 292 | 0.15 | Tide gauge (half the maximum wave height) | |||
| Diba | Oman | 494 | 0.17 | Tide gauge (half the maximum wave height) | |||
| Majis | Oman | 594 | 0.13 | Tide gauge (half the maximum wave height) | |||
| Muscat | Oman | 812 | 0.13 | Tide gauge (half the maximum wave height) | |||
| Quaryyat (Quriat) | Oman | 866 | 0.12 | Tide gauge (half the maximum wave height) | |||
| Chabahr | Iran | 907 | 0.08 | Tide gauge (half the maximum wave height) | |||
| Sur | Oman | 961 | 0.03 | Tide gauge (half the maximum wave height) |
More
Every tsunami in 2017The 2000sTsunamis of IranThis 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 5643.