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Global SRTM coupled with GEBCO, local DEMS (why, how and where with links to deliverables/products) (Gerrit/Amrit)
Correction with vegetation (why, how and where with links to deliverables/products) (Arjen Haag)
Method using water levels (why, how and where with links to deliverables/products) (Ed)
Waves
Field measurements (why, how and where with links to deliverables/products) (Iris)
Era interim, translated to nearshore depth limited waves (why, how and where with links to deliverables/products) (Kees)
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The water levels, which are a combination of tidal elevation and storm surge, have been chosen rather arbitrarily at 1, 3 and 6 m above MSL. Substantially higher levels occur are likely to occur at some places in the world. For instance, parts of Bretagne have a tidal range of well over 10 m. There, only 1 m of surge is required for MSL + 6m, which seems not extreme. The feeling is that the selected levels are representative of a large part of the world, especially areas near the equator where the application of the FAST tool seems most likely.
Diva, model Model Martin (Jasper)
Vegetation
Field data (why, how and where with links to deliverables/products) (Iris)
NDVI/LAI (why, how and where with links to deliverables/products) (Daphne)
Yes/no vegetation map (why, how and where with links to deliverables/products) (Josh)
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MI-Safe services
MI-Safe provides ....for case study sites. For other foreshore areas in the world MI-Safe reverts to ....
When a user queries a location in the Educational version of the MI-SAFE tool combines data from four parameters to assess the effect of the foreshore on wave attenuation (See Figure Below):
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