https://www.seappinc.com/about daily 1.0 2023-09-09 https://images.squarespace-cdn.com/content/v1/589213a4d1758e15f1596af6/1493236819573-A2713FJQGPOO52HT2AP1/image-asset.jpeg Company Profile https://www.seappinc.com/company-principals daily 0.75 2023-09-09 https://images.squarespace-cdn.com/content/v1/589213a4d1758e15f1596af6/1493240748587-WUB36S9UFJXW7IVXUJZ9/kim.jpg Company Principals https://images.squarespace-cdn.com/content/v1/589213a4d1758e15f1596af6/1493248159013-TW6M5V0TSXV23HWE1L7E/collage4.jpg Company Principals https://www.seappinc.com/work daily 0.75 2023-09-09 https://images.squarespace-cdn.com/content/v1/589213a4d1758e15f1596af6/1541963054761-Q0JCH8QIMS899VNQQT2O/juno+reflector+40.jpg Company Projects https://images.squarespace-cdn.com/content/v1/589213a4d1758e15f1596af6/1541966076452-8DMN3A5O7RDLJKCUMR8J/lido+ostia+60.jpg Company Projects Lido Ostia is a popular beach resort and residential area to the west of Rome, Italy and just to the south of the Tiber River Delta on the west coast of Italy. In recent years beach erosion has accelerated and threatened to impact the economy of this resort, which is a 20 minute train ride from the heart of Rome. Thus, local government and regional entities pooled resourced to complete a study to identify the optimal beach restoration and shore protection methods to return Lido Ostia to its full status as a beach resort. Following a series of conceptual designs Coastal Modeling System (CMS) of the U.S. army Corps of Engineers was used to test alternatives. The model computational grid for the Lido Ostia Project area consists of about 30,000 water cells varying in size from 30 meters to 10 meters on a side. Smaller cell sizes were required to resolve the shore protection structures in the model. Cells containing the structures were specified as harbottom, non-erodible cells. The topographic data in the model grid were set using results of a recent survey of the project area. Forcing for the model was provided by a time series of measured directional wave data that were adjusted to shallow water topography present in the Lido Ostia area. The directional wave data was input at three hour intervals and adjusted to a spectral spread of energy according to wave period. The tides were represented at the boundary of the circulation model using 15cm semidiurnal (M2) tide amplitude. https://images.squarespace-cdn.com/content/v1/589213a4d1758e15f1596af6/1541879328301-OJL6WV2PX4VSM75AX2S6/fencejupiter+borrow.jpg Company Projects