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Alma 1966 −80.5135 25.0110 0.30 Above Normal Tavernier
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Betsy 1965 −80.5148 25.0096 2.35 Mean Low Water Tavernier
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Donna 1960 −80.6353 24.9133 4.11 Upper Matecumbe Key
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Labor Day 1935 −80.7375 24.8516 5.49 Lower Matecumbe
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Unnamed 1929 −80.3885 25.1848 2.68 Mean Sea Level Key Largo
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The recurrence interval projection is by necessity based on a sparse dataset, and caution should
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be used in its interpretation. As projection intervals become longer, it is more likely that the observed
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data are inadequate to robustly represent all possibilities. Furthermore, these projections do not
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incorporate changes from sea level rise or from a changing climate, which can alter the strength and
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frequency of storms. An important aspect of sea level rise is that it significantly shortens the expected
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recurrence intervals of storm surge. For example, under a median sea level rise projection at Key West,
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J. Mar. Sci. Eng. 2017, 5, 31 23 of 26
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Park et al. [45] find that a one-in-50-year storm surge based on historic data in 2010 can be expected to
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occur once every five years by 2060.
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Figure A2. Storm surge recurrence intervals from the SurgeDat database and return period predictor
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for a 25-mile radius centered on 25.2◦ N, 80.7◦ W.
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Table A4. Recurrence interval projection in years from the Florida Bay SurgeDat data. Note that this
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projection does not take into account future sea level rise.
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Interval (Year) Surge (m) Interval (Year) Surge (m)
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10 0.45 56 3.88
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12 0.82 58 3.95
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14 1.12 60 4.02
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16 1.39 62 4.08
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18 1.62 64 4.15
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20 1.83 66 4.21
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22 2.02 68 4.27
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24 2.19 70 4.33
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26 2.35 72 4.38
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28 2.50 74 4.44
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30 2.64 76 4.49
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32 2.77 78 4.54
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34 2.89 80 4.59
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36 3.00 82 4.64
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38 3.11 84 4.69
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40 3.21 86 4.73
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42 3.31 88 4.78
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44 3.40 90 4.82
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46 3.49 92 4.87
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48 3.57 94 4.91
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50 3.65 96 4.95
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52 3.73 98 4.99
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54 3.81 100 5.03
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