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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 />

looking for opportunities for outdoor recreation. Further, as development proceeds, accessible<br />

upl<strong>and</strong> natural areas may become even rarer, concentrating this pressure into increasingly rare<br />

remnant habitats. As a result, as development proceeds, the need to manage the impacts<br />

associated with outdoor recreation will only intensify.<br />

6.3.9 Climate change<br />

Projections suggest that climate change will have significant impacts on terrestrial natural<br />

heritage features in the Lake Simcoe watershed. Recent modeling work was completed for the<br />

Lake Simcoe watershed, examining the response of tree species to climate change, as<br />

influenced through factors such as the current range of the species, its current local abundance,<br />

phenology, <strong>and</strong> seed production (Puric-Mladenovic et al., 2011). As climates change, the model<br />

predicts that balsam fir (Abies balsamea), red maple (Acer rubrum), American beech (Fagus<br />

gr<strong>and</strong>ifolia), yellow birch (Betula alleghaniensis), white cedar (Thuja occidentalis) <strong>and</strong> eastern<br />

hemlock (Tsuga canadensis) will all exhibit slight decreases in their occurrence in the forests of<br />

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. In fact, the projected<br />

shifts in climate may cause some species which are currently relatively widely distributed to<br />

become more narrowly restricted to remaining habitat, including red maple becoming restricted<br />

to wetl<strong>and</strong>s, as they shift to areas with moister soil, <strong>and</strong> yellow birch becoming restricted to<br />

ravines, as they shift to areas with cooler <strong>and</strong> moister microclimate. Other species, notably red<br />

oak (Quercus rubra), are anticipated to become more common as a result of the warming<br />

climate.<br />

Modeling results suggest that forests in cooler microclimates in ravines <strong>and</strong> north facing slopes,<br />

which tend to have a relatively high dominance of eastern hemlock, yellow birch, <strong>and</strong> American<br />

beech, may be among the most sensitive ecosystem to the changing climate. Sadly though, the<br />

species which the model suggests are the most vulnerable to climate change are those which<br />

we think of as being proto-typically Canadian. Both sugar maple (Acer saccharum) (Canada’s<br />

national symbol), <strong>and</strong> white pine (Pinus strobus) (Ontario’s provincial tree) are predicted to<br />

experience severe declines in 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 (Puric-Mladenovic et al., 2011).<br />

A separate set of models, developed to assess the vulnerability of wetl<strong>and</strong> ecosystems, suggest<br />

that a ‘worst case’ climate change scenario would have catastrophic impacts on wetl<strong>and</strong>s in the<br />

Lake Simcoe watershed. The increases in average annual temperature <strong>and</strong> decreases in<br />

average annual precipitation projected to occur by the year 2100 is estimated to make 90% of<br />

the swamps <strong>and</strong> 84% of the marshes in the Lake Simcoe watershed vulnerable to drying. As<br />

drying occurs, it is expected that marshes would shift in composition to become swamp (or<br />

thicket swamp) type communities, <strong>and</strong> treed swamps would shift to become mesic forests.<br />

Interestingly however, these same models suggest that the swamps <strong>and</strong> marshes in the <strong>Barrie</strong><br />

<strong><strong>Creek</strong>s</strong>, <strong>Lovers</strong> <strong>Creek</strong>, <strong>and</strong> Hewitt’s <strong>Creek</strong> subwatersheds will be more resilient to projected<br />

changes in climate, due to the role of ground water discharge in maintaining these wetl<strong>and</strong><br />

features (Chu, 2011).<br />

In sum, these models suggest that there will be a shift in community composition in the natural<br />

areas in 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, <strong>and</strong> a net loss of<br />

tree species diversity. Unfortunately, natural areas lacking in biodiversity tend to be more<br />

vulnerable to other threats such as insects, disease, <strong>and</strong> invasive species, suggesting that the<br />

impacts seen to terrestrial natural heritage features may become cumulative in nature.<br />

This loss in native tree species diversity may be mitigated somewhat by the ability of species<br />

not currently found here to thrive in the expected new climate. Species found in southern<br />

Chapter 6: Terrestrial Natural Heritage 295

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