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Ontario Power Generation's Response to the Joint Review

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Attachment 1 <strong>to</strong> OPG letter, Albert Sweetnam <strong>to</strong> Dr. Stella Swanson, “Deep Geologic Reposi<strong>to</strong>ry Project for Low and Intermediate Level Waste – Submission of<br />

<strong>Response</strong>s <strong>to</strong> <strong>the</strong> Final Sub-set of Package #4 Information Requests”, CD#: 00216-CORR-00531-00143.<br />

IR# EIS Guidelines<br />

Section<br />

The response is provided in two parts:<br />

a) Precipitation intensity; and<br />

b) Probable Maximum Precipitation.<br />

Information Request and <strong>Response</strong><br />

(a) Precipitation Intensity<br />

The DGR environmental assessment (GOLDER 2011, Appendix D, Section D2.3.4) considers changes in climate<br />

within <strong>the</strong> Great Lakes Basin, specifically changes in both mean precipitation and precipitation intensity. Forecasts<br />

from <strong>the</strong> Intergovernmental Panel on Climate Change (IPCC), and recent papers by Warren et al. (2004), Mortsch et al.<br />

(2003) and Kharin et al. (2007) were cited and <strong>the</strong> information presented. It was noted that Kharin et al. (2007)<br />

suggests <strong>the</strong> 20-year return period for <strong>to</strong>tal 24-hour rainfall could increase in intensity by 10% <strong>to</strong> 20% by <strong>the</strong> 2071 <strong>to</strong><br />

2100 forecast period.<br />

With respect <strong>to</strong> <strong>the</strong> Information Request for an updated evaluation, <strong>the</strong> literature was surveyed for recent literature on<br />

precipitation intensity relevant <strong>to</strong> sou<strong>the</strong>rn <strong>Ontario</strong>, and one new paper was identified:<br />

Cheng et al. (2011) suggest an increase in frequency of future daily heavy rainfall events over <strong>the</strong> period 2081<br />

<strong>to</strong> 2100 for four river basins in sou<strong>the</strong>rn <strong>Ontario</strong>. Cheng et al. (2011) also predict increases in <strong>the</strong> return values<br />

of annual maximum 3-day accumulated rainfall. More specifically, for <strong>the</strong> 100-year return period s<strong>to</strong>rm<br />

(considered in <strong>the</strong> DGR s<strong>to</strong>rmwater management design), <strong>the</strong> 3-day accumulated rainfall <strong>to</strong>tals are projected <strong>to</strong><br />

increase from about 100 mm currently observed <strong>to</strong> 130-170 mm for <strong>the</strong> period 2051-2100. The 24-hour<br />

accumulated rainfall would be less than Cheng’s 3-day accumulated rainfall projection, but is not estimated in<br />

<strong>the</strong> paper.<br />

As outlined in OPG’s response <strong>to</strong> IR-EIS-04-130, <strong>the</strong> s<strong>to</strong>rmwater management pond is designed <strong>to</strong>:<br />

� provide a minimum retention time of 24 hours for runoff from 25 mm of rainfall in 6 hours;<br />

� ensure that <strong>the</strong> average annual <strong>to</strong>tal suspended solids concentration in effluent discharge does not exceed<br />

40 mg/L;<br />

� attenuate post-development peak outflow rates for 24-hour rainfall events with return periods ranging from 2 <strong>to</strong><br />

100 years <strong>to</strong> pre-development values; and<br />

� safely convey <strong>the</strong> peak outflow rate from <strong>the</strong> 24-hour, 100-year rainfall event.<br />

The current design of <strong>the</strong> s<strong>to</strong>rmwater management pond considers a 24-hour rainfall event with a return period of<br />

100 years (110 mm) based on data from Goderich, <strong>Ontario</strong>. As stated in <strong>the</strong> response <strong>to</strong> IR-EIS-04-130, it is expected<br />

that <strong>the</strong> rainfall amounts at Kincardine would be less than at Goderich. The design of <strong>the</strong> s<strong>to</strong>rmwater management<br />

pond has extra capacity if rainfall intensity is higher, in part because of conservative assumptions leading <strong>to</strong> <strong>the</strong> current<br />

design and <strong>the</strong> availability of 300 mm of planned freeboard on <strong>the</strong> sides of <strong>the</strong> pond. The capability of downstream<br />

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