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Flood Risk and Vulnerability Analysis Project - Atlantic Climate ...

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Return Periods (years)<br />

Duration 2 5 10 20 25 50 100<br />

5 min 4.4 6.3 7.6 8.8 9.2 10.4 11.5<br />

10 min 6.5 9.4 11.2 10.8 13.6 15.4 17.1<br />

15 min 7.8 11.3 13.6 15.9 16.6 18.7 20.9<br />

30 min 10.4 15.2 18.4 21.5 22.5 25.5 28.5<br />

1 h 13.3 18.4 21.7 24.9 25.9 29.0 32.1<br />

2 h 18.3 23.7 27.4 30.8 31.9 35.3 38.7<br />

6 h 30.1 37.9 43.1 48.1 49.7 54.5 59.3<br />

12 h 38.7 49.0 55.8 62.3 64.3 70.7 77.0<br />

24 h 47.3 62.4 72.4 82.0 85.0 94.4 103.7<br />

Table 3-10. Updated IDF values for G<strong>and</strong>er based on data to 2011<br />

Return Period (years)<br />

Duration 2 5 10 20 25 50 100<br />

5 min 3.9 5.6 6.6 7.6 8.0 9.0 10.0<br />

10 min 5.7 8.5 10.3 12.1 12.7 14.4 16.1<br />

15 min 6.9 10.3 12.6 14.8 15.5 17.7 19.8<br />

30 min 8.8 13.3 16.3 19.2 20.1 22.9 25.7<br />

1 h 11.2 15.7 18.6 21.5 22.4 25.2 27.9<br />

2 h 14.5 19.5 22.8 26.0 27.0 30.1 33.2<br />

6 h 24.1 31.1 35.7 40.2 41.6 45.9 50.2<br />

12 h 32.1 40.3 45.8 51.0 52.7 57.8 62.9<br />

24 h 40.7 51.4 58.4 65.2 67.4 74.0 80.6<br />

Table 3-11. Updated IDF values for Goose Bay based on data to 2009<br />

except for 24-hr precipitation which is to 2011.<br />

In a concurrent study conducted by AMEC, IDF values were projected into the future (2020,<br />

2050 <strong>and</strong> 2080) for St. John‟s, Stephenville <strong>and</strong> Deer Lake, all on the isl<strong>and</strong> of Newfoundl<strong>and</strong>.<br />

At the 24 hr duration the IDF values for Deer Lake <strong>and</strong> Stephenville (both in WRMD‟s West<br />

Region) increased by a greater amount than St. John‟s (WRMD East Region). IDF values at a<br />

24 hr duration for Deer Lake increased from 2-4 % in 2020 to 4-7 % in 2080. The IDF values for<br />

Stephenville showed consistent increases near 4-10 %. However, the 24 hr duration IDF values<br />

for St. John‟s only increased from 1 % in 2020 to 2-4 % in 2080. While the scale of increase<br />

may not precisely match the values given in Table 3-8, they are not inconceivable considering<br />

the values in Table 3-8 are for much larger geographical area versus points <strong>and</strong> for only two<br />

seasons using a somewhat conservative SRES scenario (A2). Also, the increase in precipitation<br />

at Deer Lake <strong>and</strong> Stephenville compared to St. John‟s is captured in the West vs. East region<br />

(respectively) values.<br />

TA1112733 page 58

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