  The lack of offshore seismic data caused uncertainties associated to
understating the behavior of future tsunamigenic earthquakes in the Makran
Subduction Zone (MSZ). Future tsunamigenic events in the MSZ may trigger
significant near-field tsunamis. Run-up heights in the near-field are
controlled by the heterogeneity of slip over the rupture area. Considering a
non-planar geometry for the Makran subduction zone, a range of random k^{-2}
slip models were generated to hypothesize rupturing on the fault zone. We model
tsunamis numerically and assess probabilistic tsunami hazard in the near-field
for all synthetic scenarios. The main affected areas by tsunami waves are the
area between Jask and Ormara along the shorelines of Iran and Pakistan and the
area between Muscat and Sur along the Oman coastline. The maximum peak-run-up
along the shores of Iran and Pakistan is about 16 m and about 12 m for the Oman
shoreline. The slip distributions control the run-up along the Makran
coastlines. The dependency of run-up to the heterogeneity of slip is higher in
the most impacted areas. Those areas are more vulnerable to tsunami hazard than
other areas.
