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Barrie Creeks, Lovers Creek, and Hewitt's Creek Subwatershed Plan

Barrie Creeks, Lovers Creek, and Hewitt's Creek Subwatershed Plan

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The <strong>Barrie</strong> <strong><strong>Creek</strong>s</strong>, <strong>Lovers</strong> <strong>Creek</strong> <strong>and</strong> Hewitt’s <strong>Creek</strong> <strong>Subwatershed</strong> <strong>Plan</strong><br />

4.4.3 Climate<br />

The climate of the <strong>Barrie</strong> <strong><strong>Creek</strong>s</strong>, <strong>Lovers</strong> <strong>Creek</strong>, <strong>and</strong> Hewitt’s <strong>Creek</strong> subwatersheds directly<br />

determines the quantity of surface <strong>and</strong> groundwater present in the system. When the spring<br />

melt occurs, a large volume of water is released. This water will first infiltrate the ground. When<br />

the soil becomes supersaturated the remaining water will flow overl<strong>and</strong> until it reaches the<br />

tributaries <strong>and</strong> main branch of the river.<br />

The temperature in the subwatershed can directly affect the quantity of water present in the<br />

system. In the cold winter months the water is frozen at the surface so the quantity of available<br />

water is reduced. In the hot summer months the water is flowing but an overall loss is occurring<br />

due to the high rates of evaporation.<br />

4.4.4 Water Budget Stress Assessments<br />

Potential water quantity stress is being estimated on a subwatershed scale through the Source<br />

Protection <strong>Plan</strong>ning process. Several water budget initiatives have been undertaken to identify<br />

potential water quantity stress within the subwatershed. The indicators of stress presented in<br />

this report are based on these studies <strong>and</strong> more information can be obtained from the following<br />

reports; SGBLS (2009), AquaResources <strong>and</strong> Golder (2010), <strong>and</strong> AquaResources et al. (2010).<br />

Tier 1 Water Budget Results<br />

The Tier 1 Water Budget Study (LSRCA, 2009) conducted a comparison of current conditions<br />

<strong>and</strong> future dem<strong>and</strong>, on both an average annual <strong>and</strong> monthly basis. The completion of the<br />

analysis helps to determine whether stress on the groundwater <strong>and</strong> surface water resources<br />

can be anticipated under various scenarios. The stress assessment evaluates the ratio of the<br />

consumptive dem<strong>and</strong> for permitted <strong>and</strong> non-permitted users to water supplies, minus water<br />

reserves, within each subwatershed (equation shown in following blue text box). The major<br />

components of the water budget have been estimated <strong>and</strong> tabulated as described in the<br />

preceding sections, including water supply, water dem<strong>and</strong>, <strong>and</strong> water reserve.<br />

Results of the current <strong>and</strong> future groundwater stress assessment using annual average dem<strong>and</strong><br />

are shown in Table 4-17 <strong>and</strong> Table 4-18. Both Hewitt’s <strong>and</strong> <strong>Lovers</strong> <strong><strong>Creek</strong>s</strong> were found not to be<br />

stressed with regard to average annual stress for current dem<strong>and</strong>, while <strong>Barrie</strong> <strong><strong>Creek</strong>s</strong> was<br />

found to have a significant potential for stress. For future dem<strong>and</strong> Hewitt’s <strong>Creek</strong> subwatershed<br />

was found to have a moderate potential for stress, while <strong>Barrie</strong> <strong><strong>Creek</strong>s</strong> maintained the<br />

significant potential for stress.<br />

Results of the current monthly surface <strong>and</strong> groundwater stress assessments are shown in Table<br />

4-19. Only <strong>Barrie</strong> <strong><strong>Creek</strong>s</strong> were found to have a potential for stress with regard to groundwater<br />

on a monthly basis. The lack of seasonal changes in stress levels are a result of a fairly<br />

consistent groundwater supply <strong>and</strong> consistent municipal pumping for water supply, which makes<br />

up the majority of water dem<strong>and</strong>.<br />

Overall, the results provide a reasonable assessment of the annual groundwater <strong>and</strong> monthly<br />

surface <strong>and</strong> groundwater supply <strong>and</strong> dem<strong>and</strong> conditions. As a result of the current <strong>and</strong> future<br />

average annual stress assessment the <strong>Barrie</strong> <strong><strong>Creek</strong>s</strong>, <strong>Lovers</strong> <strong>Creek</strong>, <strong>and</strong> Hewitt’s <strong>Creek</strong><br />

subwatersheds advanced to a Tier 2 assessment per the Clean Water Act Technical Rules. The<br />

following sections will discuss the results of the <strong>Barrie</strong> <strong><strong>Creek</strong>s</strong>, <strong>Lovers</strong> <strong>Creek</strong>, <strong>and</strong> Hewitt’s<br />

<strong>Creek</strong> Tier 2 Water Budget.<br />

Chapter 4: Water Quantity – Surface <strong>and</strong> Groundwater 193

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