A Tsunami approaching the Seychelles
The results shown on this page present the surface elevation and current
patterns caused by a propagating tsunami wave which was simulated by means of a
The model area with the bottom topography is shown below.
The area covers the islands Mahé, La Digue,
the shallow shelf, and the deep sea around the shelf.
The simulation is based on the assumption that an initial earthquake happened
close to the Nicobar Islands and generates a tsunami. The associated wave
propagates with high speed towards the Seychelles Islands and reaches
the border of the model area at the north-east boundery with a waveheight of
50 cm at model-time = 0.
Now the powerfull wave is more and more influenced by the structures of the
shallow shelf region. The model simulation confirms the assumption that
150 to 200 km apart from La Digue Island, close to the rim of the shelf
at model-time = 72 min, significant structures (variance in amount and
direction) appear in the current field,
cf. Fig. 1.
The extreme changes in the current field and the clearly marked allignment
with the isobaths can be used as an indictor for an approaching tsunami.
From now on it takes roughly 100 minutes for the first tsunami wave to reach
the coast of La Digue Island which corresponds to lead times of the same
order of magnitude.
Fig. 2 shows the corresponding
pattern in the current field at model-time = 166 min. If the simulation
proceeds another 30 minutes the larger island Mahé is stroken by the
first tsunami caused waves.
The model results presented above show current fields
with speeds up to 2 m/s which provide some evidence that such features can
be most probably be detected and tracked by HF-radar, presumed, that the radar
technology allows for sufficient short integration times (roughly 4-5 minutes)
which is possible with WERA. Further investigations will be conducted in the
The model has been set-up and run by
in cooperation with