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representing the 99-hr time sequences for each of the 16 tropical storm events
and the 144-hr time sequences for each of the 38 extratropical storm events were
input to LTFATE.
Model simulations
The six Mud Dump ambient depth/mound height combinations were sub-
jected to the 64 tropical storm surge hydrographs (16 storms times four possible
tide phases) to evaluate the erosion potential of the configurations shown in
Table G4. An identical procedure was followed for the 152 extratropical storm
surge hydrographs (38 storms times four possible tide phases). In all six simula-
tions for each type of storm, the maximum vertical erosion experienced at any
location on the mound during each of the simulations was archived for use in the
EST to develop vertical erosion versus frequency-of-occurrence relationships.
EST Input File Development
As noted earlier, EST is a statistical procedure that uses a limited database of
historical occurrences to generate multiple simulated scenarios from which fre-
quency relationships and error estimates can be computed. The EST requires
two types of input. The first set represents descriptive storm parameters that
define the dynamics of each storm event. These parameters, referred to as input
vectors, should be (a) tidal phase, (b) duration of the event measured as the
number of hours during which the computed transport magnitude exceeds 10.0
storm event, (d) wave height, (e) wave period, and (f) maximum depth-averaged
velocity magnitude associated with the maximum transport value.
The second input parameter represents a measure of damage resulting from
the passage of the storm event. These parameters are referred to as response
vectors. Typical response vectors are storm surge elevation, shoreline erosion,
dune recession, flood inundation, or for capping projects, vertical erosion.
Tropical storm vectors
Input and response vectors for hurricanes #296, 327, 748, and 835 for high
water after flood (maximum tidal surface elevation) for the site scenario of an
8-ft mound located in 83 ft of water are shown in Table G6.
The EST uses the parameters of Table G6 for all tropical storm events and
each of the four tidal phases as a basis for simulating multiple repetitions of
multiple years of storm activity. In this application, 100 repetitions of a 200-year
sequence of storm activity were simulated for the six scenarios shown in
Table G6. As mentioned above, the EST assumes that future storm activity will
be similar to past events, i.e., a hurricane such as Camille, which devastated the
G21
Appendix G Procedures for Conducting Frequency-of-Erosion Studies
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