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<br />Floodwaters need not be deep or fast to affecl <br />the integrity of an anchoring system, Soil satura, <br />tion occurring during periods of prolonged flooding <br />can reduce the holding capacity of ground anchors <br />causing them to pull out as shown in Figure 1,25, <br /> <br /> <br />Figure 1.25 Failed Ground Anchor <br /> <br />Deep flooding accentuates the forces acting <br />upon the foundation and anchoring systems of a <br />manufactured home, In addition, increased flood <br />depths affect a non-elevated manufactured home <br />by directly transferring forces to the walls and floor, <br />The initial imbalance of water levels between the <br />exterior and interior of the manufactured home will <br />likely result in buoyancy. This uplift force can com- <br />pletely dislodge an inadequately anchored <br />manufactured home from its foundation, This <br />typically occurs in fast rising waters or when the <br />rate-of-rise' of floodwaters is very fast. <br />In situations where the rate-of-rise of floodwaters <br />is slow, allowing the manufactured home to fill with <br />water and therefore counteracting the buoyancy <br />forces, or where adequate anchoring is employed <br />to resist dislodging the manufactured home from <br />its foundation, deep flooding can substantially <br />damage a non-elevated manufactured home by <br />direct inundation, Although the manufactured <br />home may remain in place, as shown in Figure <br />1,26, it will likely be a total loss due to the damage <br />caused by water inundation, <br /> <br /> <br />Figure 1.26 Deep Flooding Damage <br /> <br />In addition to having high erosion and scour <br />potential, deep velocity flooding also emphasizes <br />the need to consider debris impact potential. <br />Coastal Flooding-Coastal flooding is generally <br />due to ocean-based storm systems, Hurricanes, <br />tropical storms, and extratropical storms, such as <br />"northeasters," are the principal causes, with <br />flooding occurring when storm tides are much <br />higher than the normal tide, This is a "storm <br />surge" and exhibits high water velocity and wave <br />action, The maximum intensity of a storm tide oc- <br />curs at high tide, so storms that persist through <br />several tide cycles, such as "northeasters," are <br />the most severe, <br />The velocity and range of coastal floods vary in <br />part with the severity of the storm of which they <br />are a part, The damaging effects of coastal <br />flooding are caused by a combination of the storm <br />surge, rain, wind, waves, erosion, and battering <br />by debris, <br />The extent and nature of coastal flooding is also <br />related to physiographic features of the terrain and <br />the characteristics of the adjoining body of water. <br />Pacific coastal areas are principally vulnerable to <br />earthquakes, tsunamis (seismically induced tidal <br />waves) and other natural forces that can trigger <br />excessive erosion, mud slides, and flash flooding, <br />Great Lakes coastal areas are subject to erosion <br />and severe winter storms. The Atlantic and Gulf <br />Coasts are consistently exposed to the forces of <br />hurricanes, lesser tropical storms, and <br />northeasters, <br /> <br />10 <br />