Abstract:
The presence of ionospheric disturbances associated with Sumatra 2004 tsunami that
propagated ahead of tsunami itself has previously been identified. However, their origin remains
unresolved till date. Focusing on their origin mechanism, we document these ionospheric disturbances
referred as Ahead of tsunami Traveling Ionospheric Disturbances (ATIDs). Using total electron content (TEC)
data from GPS Aided GEO Augmented Navigation GPS receivers located near the Indian east coast, we first
confirm the ATIDs presence in TEC that appear ~90 min ahead of the arrival of tsunami at the Indian east
coast. We propose here a simulation study based on tsunami-atmospheric-ionospheric coupling that
considers tsunamigenic acoustic gravity waves (AGWs) to excite these disturbances. We explain the ATIDs
generation based on the dissipation of transverse mode of the primary AGWs. The simulation corroborates
the excitation of ATIDs with characteristics similar to the observations. Therefore, we offer an alternative
theoretical tool to monitor the offshore ATIDs where observations are either rare or not available and could
be potentially important for the tsunami early warning.