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This study evaluated the individual drag force model (iDFM), a subgrid-scale model for simulating tsunami inundation in coastal urban areas. The iDFM was then applied to characterize Typhoon Haiyan-induced storm surge inundations in 2013. Using a post-typhoon survey dataset containing inundation depths at different survey points with inundation limits, the performance of iDFM was validated, and the results confirmed that iDFM accurately estimates the storm surge inundation depths but overestimates the limit of inundation. In addition, the results revealed that the iDFM flow velocity was a dominant factor, and the inclusion of buildings in the simulated affected the arrival of the leading edge of inundation. Furthermore, the reduction in flow velocity was sensitive to the subgrid-scale parameters, and the spatial distribution pattern of buildings located in the inundated area affected the relative difference in the maximum flow velocity with the regional roughness model. The inundation characteristics of the Typhoon Haiyan storm surge models were compared with a historical tsunami event. The inundation characteristics were similar and model differences were observed mainly in the fluid velocity and momentum flux rather than the inundation depth. However, the magnitudes of relative differences observed in Tacloban were larger for fluid velocity and momentum flux, respectively, than in the tsunami event. The effect of building drag on advection was also substantial in Tacloban due to the differences in the inflow mass and momentum fluxes. • This study applys a subgrid-scale model of the tsunami inundation in a coastal urban area, called the individual drag force model (iDFM), to Typhoon Haiyan-induced storm surge inundations in 2013. The accuracy of iDFM is validated in comparison with the post-survey dataset, measuring inundation depths at survey points and the limit of inundation. In addition, the characteristics of the modeled inundation flow by the iDFM are examined by comparing them with the characteristics of the regional roughness model corresponding to the land use category. Moreover, the similarities and differences in the inundation characteristics are compared with a historical tsunami event in the authors' previous publication. [ABSTRACT FROM AUTHOR]