Tsunami Arrival Time Calculator

Find how long a tsunami takes to cross an ocean path with changing depth, when it arrives on the clock, and how much warning time you have.

🌊 Tsunami Arrival Time Calculator
Path segmentslength (km) and mean depth (m), up to 5 rows
Length (km)
Mean depth (m)
Source and receiverdegrees, negative for south and west
Source latitude
Source longitude
Receiver latitude
Receiver longitude
Mean ocean depth
m
1008000
Origin time (UTC)hour (0 to 23) and minute (0 to 59)
Alert delay after the earthquake
min
0120
Time needed to evacuate
min
0600
Total travel time
—
Arrival (UTC)
—
Travel time in hours
—
Path length
—
Average speed
—
Warning time after alert
—
Margin over evacuation time
—

🌊 What is Tsunami Arrival Time?

Tsunami arrival time is the time a tsunami takes to travel from its source, usually an undersea earthquake, to a particular coast, and the clock time at which its first wave reaches that coast. Because a tsunami is a very long wave, its speed in the ocean depends only on the water depth: the deeper the water, the faster it moves. In the open ocean it travels at jet-aircraft speed, around 700 to 800 km/h, and then slows to the speed of a car as it climbs onto a continental shelf. Adding up the time spent in each depth zone gives the arrival time.

Emergency planners, coastal engineers, students and journalists use arrival times to answer practical questions. How many hours does a distant-source tsunami give a harbour before the first wave? Is there enough time for vertical or inland evacuation? Which stretch of a path adds the most delay? Warning centres use detailed numerical models for official forecasts, but a segment-by-segment estimate such as this one is how the basic travel-time maps and rules of thumb are built, and it is an excellent way to understand why a wave from Chile takes about 15 hours to reach Hawaii while a wave from a shelf-edge earthquake can arrive in minutes.

This page adds the multi-depth path, the cumulative time and the arrival clock time to the single-depth speed formula. In Depth path mode you enter up to 5 segments, each with a length in kilometres and a mean depth in metres. In Great-circle mode you enter source and receiver coordinates and one mean depth, and the distance is found with the haversine formula. In both modes you can enter an alert delay and an evacuation time to see the warning time left and the margin. For the speed on its own see the tsunami wave speed calculator, and for the height of the wave at the shore see the tsunami run-up height estimator.

Two misconceptions are worth avoiding. A tsunami is not a single wave but a train of waves, and the first wave is often not the largest, so the arrival time here marks the start of the danger, not its end. And the estimate is an approximation: the real wave front bends toward shallower water (refraction), the source is a long rupture rather than a point, and the seabed is far more complicated than five straight segments. Use the result to understand the scale of the time available, never as the only basis for a safety decision. Follow official warnings.

📐 Formula

ci  =  √(g × hi)   |   ti  =  Li ÷ ci   |   T  =  Σ ti
g = standard gravity, 9.80665 m/s².
hi = mean ocean depth of segment i (m). The shallow-water speed is valid because a tsunami wavelength is much greater than the depth.
Li = length of segment i (m, entered in km). ci = wave speed (m/s). ti = segment time (s).
T = total travel time. Arrival clock time = origin time + T. Warning time = T − alert delay. Margin = warning time − evacuation time.
Great-circle distance: d = 2R × arcsin(√(sin²(Δφ/2) + cos φ1 cos φ2 sin²(Δλ/2))), with R = 6371 km, then T = d ÷ √(g h).
Example: h = 4000 m gives c = √(9.80665 × 4000) = 198.1 m/s, so 1000 km takes 1,000,000 ÷ 198.06 = 5049 s, or 1 h 24 min.

📖 How to Use This Calculator

Steps

1
Choose a mode. Pick Depth path to enter up to 5 segments with their own length and mean depth, or Great-circle to enter source and receiver coordinates and one mean depth.
2
Enter the path and the origin time. Type segment lengths in kilometres and mean depths in metres (leave unused rows blank), or the latitudes and longitudes. Set the origin hour and minute in UTC.
3
Add alert delay and evacuation time. Enter the minutes before an alert is issued and the minutes people need to evacuate to see the warning time and margin.
4
Read the arrival time and chart. The calculator gives total travel time, average speed, arrival clock time with the day offset, and a chart of cumulative time against distance or of time against mean depth.

💡 Example Calculations

Example 1 — Pacific Crossing, Chile to Hawaii (Great-circle)

Source 38.2°S 73.05°W (off Chile), receiver 19.73°N 155.09°W (Hilo, Hawaii), mean depth 4000 m, origin 19:11 UTC

1
Haversine distance with R = 6371 km: d = 10,686 km.
2
Wave speed: c = √(9.80665 × 4000) = 198.1 m/s (713 km/h).
3
Time = 10,686,251 m ÷ 198.1 m/s = 53,955 s = 899.3 min = 14.99 h. Added to 19:11 UTC this is 10:10 UTC the next day.
4
With a 15 min alert delay the warning time is 14 h 44 min, and with 120 min needed to evacuate the margin is +12 h 44 min.
Travel time = 14 h 59 min, arrival = 10:10 UTC (+1 day), average speed 198.1 m/s
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Example 2 — Japan 2011 to Hawaii (Depth path)

Five segments, 6300 km in total, mostly 5400 m deep, origin 05:46 UTC, alert delay 20 min, evacuation 60 min

1
Near-source shelf and slope: 120 km at 1500 m takes 16 min, and 300 km at 5500 m takes 22 min.
2
Open Pacific: 5500 km at 5400 m has c = 230.1 m/s and takes 6 h 38 min.
3
Approach to the islands: 250 km at 4500 m takes 20 min and 130 km at 1000 m takes 22 min.
4
Total = 478.1 min = 7 h 58 min, so arrival is 13:44 UTC on the same day. Warning time is 7 h 38 min and the margin is +6 h 38 min.
Travel time = 7 h 58 min, arrival = 13:44 UTC, average speed 219.6 m/s. This is in the same range as the 7 to 8 hours reported for the 2011 event, but the depths here are illustrative, not a reconstruction.
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Example 3 — Short Continental Shelf Path (Depth path)

A 200 km path from the shelf edge to the coast, origin 03:30 UTC, alert delay 10 min, evacuation 30 min

1
Slope: 60 km at 2500 m (c = 156.6 m/s) takes 6 min, and 40 km at 800 m (c = 88.6 m/s) takes 8 min.
2
Shelf: 50 km at 200 m (c = 44.3 m/s) takes 19 min, and 30 km at 100 m (c = 31.3 m/s) takes 16 min.
3
Coastal zone: 20 km at 40 m (c = 19.8 m/s) takes 17 min.
4
Total = 65.5 min = 1 h 6 min, arrival 04:36 UTC. Warning time is 56 min, so the margin over a 30 min evacuation is +26 min.
Travel time = 1 h 6 min, arrival = 04:36 UTC, average speed 50.9 m/s (183 km/h)
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Example 4 — Shallow Segments Near the Coast (Depth path)

2030 km path, deep ocean then a shelf that shallows to 20 m, origin 12:00 UTC, alert delay 10 min, evacuation 45 min

1
Deep ocean: 1500 km at 4000 m (c = 198.1 m/s) takes 2 h 6 min.
2
Slope: 300 km at 1500 m takes 41 min, and 150 km at 500 m takes 36 min.
3
Shelf: 60 km at 100 m takes 32 min, and the last 20 km at 20 m (c = 14.0 m/s) takes 24 min.
4
The last 80 km is only 4 percent of the distance but takes 56 min, over 21 percent of the 4 h 19 min total. Arrival is 16:19 UTC, warning time is 4 h 9 min and the margin is +3 h 24 min.
Travel time = 4 h 19 min, arrival = 16:19 UTC, average speed 130.7 m/s (470 km/h)
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❓ Frequently Asked Questions

How do you calculate tsunami arrival time?+
Divide the path into segments of roughly constant depth. For each, the wave speed is c = sqrt(g h) with g = 9.80665 m/s squared, and the time is length divided by speed. Add the segment times to get the total, then add it to the origin time to get the arrival clock time.
How fast does a tsunami travel in the deep ocean?+
In 4000 m of water the speed is sqrt(9.80665 x 4000) = 198 m/s, about 713 km/h, close to a passenger jet. In 5000 m it is about 221 m/s or 797 km/h. NOAA describes deep-ocean tsunami speeds as comparable to a jet plane.
Why does a tsunami slow down near the coast?+
Speed depends on depth, c = sqrt(g h). When the water shoals from 4000 m to 10 m the speed drops from about 198 m/s to about 10 m/s, roughly the speed of a car. The wave height grows as the speed falls because the energy is compressed.
Is the shallow-water formula valid for a tsunami in deep ocean?+
Yes. A tsunami wavelength is tens to hundreds of kilometres, far longer than even the deepest ocean, so the water is shallow relative to the wave. That is why c = sqrt(g h) works, unlike for wind waves, whose speed depends on wavelength.
How long does a tsunami take to cross the Pacific?+
Roughly 15 hours from Chile to Hawaii, about 10,700 km at an average depth near 4000 m. Crossing the full ocean from east to west takes about a day. Observed arrivals differ from simple estimates because of real bathymetry and the path taken.
What is tsunami warning time?+
It is the time between an official alert and the arrival of the first wave. Here it equals total travel time minus the alert delay. Comparing it with the time needed to evacuate shows whether people at a given coast can reach safety in time.
How accurate is this tsunami travel time estimate?+
Within about 5 to 10 percent for open-ocean paths when you choose representative depths. Errors grow near the coast, where depth changes quickly, and from the source region, which is not a point. Operational centres use full bathymetric models for official forecasts.
Why use a great-circle distance?+
The shortest route over a sphere is the great circle, computed here with the haversine formula and Earth radius 6371 km. A real tsunami bends toward shallower water and around islands, so the actual path is usually a little longer than the great circle.
What mean depth should I use for the open ocean?+
Use about 4000 m for a typical Pacific or Atlantic crossing, since average ocean depth is about 3700 m and abyssal plains are 4000 to 6000 m. Over a continental shelf use 50 to 200 m, and in a trench region use the local chart depth.
What does +1 day mean in the arrival time?+
It means the tsunami arrives on the calendar day after the origin time in UTC. For example, an origin at 19:11 UTC with a 15 hour travel time arrives at 10:10 UTC the next day, shown as 10:10 UTC (+1 day). Convert to local time yourself.
Does a bigger earthquake make the tsunami arrive sooner?+
No. Arrival time depends on distance and water depth, not on the size of the source. A larger earthquake makes a bigger tsunami with a larger run-up, but the first wave front still travels at sqrt(g h) along the same path.

How do you calculate tsunami arrival time?

Divide the path into segments of roughly constant depth. For each, the wave speed is c = sqrt(g h) with g = 9.80665 m/s squared, and the time is length divided by speed. Add the segment times to get the total, then add it to the origin time to get the arrival clock time.

How fast does a tsunami travel in the deep ocean?

In 4000 m of water the speed is sqrt(9.80665 x 4000) = 198 m/s, about 713 km/h, close to a passenger jet. In 5000 m it is about 221 m/s or 797 km/h. NOAA describes deep-ocean tsunami speeds as comparable to a jet plane.

Why does a tsunami slow down near the coast?

Speed depends on depth, c = sqrt(g h). When the water shoals from 4000 m to 10 m the speed drops from about 198 m/s to about 10 m/s, roughly the speed of a car. The wave height grows as the speed falls because the energy is compressed.

Is the shallow-water formula valid for a tsunami in deep ocean?

Yes. A tsunami wavelength is tens to hundreds of kilometres, far longer than even the deepest ocean, so the water is shallow relative to the wave. That is why c = sqrt(g h) works, unlike for wind waves, whose speed depends on wavelength.

How long does a tsunami take to cross the Pacific?

Roughly 15 hours from Chile to Hawaii, about 10,700 km at an average depth near 4000 m. Crossing the full ocean from east to west takes about a day. Observed arrivals differ from simple estimates because of real bathymetry and the path taken.

What is tsunami warning time?

It is the time between an official alert and the arrival of the first wave. Here it equals total travel time minus the alert delay. Comparing it with the time needed to evacuate shows whether people at a given coast can reach safety in time.

How accurate is this tsunami travel time estimate?

Within about 5 to 10 percent for open-ocean paths when you choose representative depths. Errors grow near the coast, where depth changes quickly, and from the source region, which is not a point. Operational centres use full bathymetric models for official forecasts.

Why use a great-circle distance?

The shortest route over a sphere is the great circle, computed here with the haversine formula and Earth radius 6371 km. A real tsunami bends toward shallower water and around islands, so the actual path is usually a little longer than the great circle.

What mean depth should I use for the open ocean?

Use about 4000 m for a typical Pacific or Atlantic crossing, since average ocean depth is about 3700 m and abyssal plains are 4000 to 6000 m. Over a continental shelf use 50 to 200 m, and in a trench region use the local chart depth.

What does +1 day mean in the arrival time?

It means the tsunami arrives on the calendar day after the origin time in UTC. For example, an origin at 19:11 UTC with a 15 hour travel time arrives at 10:10 UTC the next day, shown as 10:10 UTC (+1 day). Convert to local time yourself.