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In this study, ADCIRC is configured to run using a test mesh based on the Shinnecock Inlet on the Outer Barrier of Long Island, NY, USA. External forcing for the model is given by tidal forcing reconstructed from the TPXO9.1 harmonic tidal constituents using OceanMesh2D, constant air pressure of 1013 millibars, and free surface stress from winds computed from a 0.25 deg hourly CFSv2 10-m wind fields for a period of 16 days (29 December 2017 - 31 January 2018). Winds are modified for the purposes of the numerical experiment to simulate a more extreme (Category 4) event, with winds scaled radially down to zero from the point of interest, i.e. the center of the inlet (see figure in figures folder). Water elevation at an artificial recording station inside the inlet was recorded over a period of 14 days (1 January 2018 - 14 January 2018) at 3 hour intervals for different wind drag parameter samples. These water elevation values and wind drag parameters, compiled into a singular dataset, is then used to solve inverse problems.