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Cell Descriptions - South East Natural Resources Management Board

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SE6 – Lake Bonney SE<br />

NOTE: the advice below is indicative of likely change and the direction of change, with<br />

implications for ecosystems. Dates, amounts and probabilities cannot be accurately calculated at<br />

this time. Thus advice on flood levels, for example, should not be used in engineering or<br />

development planning.<br />

Climate change<br />

element/ scenario<br />

Combined<br />

climate changes<br />

and sea level rise<br />

throughout this<br />

cell<br />

Sea level rise:<br />

2030 : +c.20cm<br />

2070: +c.80cm.<br />

Storms:<br />

Frequency continues<br />

to show great<br />

variation on a<br />

decadal scale.<br />

Intensity of large<br />

storms increases.<br />

Warmer average<br />

conditions:<br />

2030:+0.3 to.6 0 C<br />

2070:+1.5 to 2 0 C<br />

Drier average<br />

conditions:<br />

2030: -2% to 5%<br />

2070: - 10% to 20%<br />

‘Flashy’ run off:<br />

Drier creeks, but<br />

larger rare floods<br />

Groundwater<br />

lowering; saline<br />

incursion:<br />

Impacts and implications Protect and manage Address landscape<br />

(for this cell) habitat threats issues: fire,<br />

connectivity,<br />

refuges, hydrology<br />

This cell presents a<br />

complex pattern of habitats<br />

sensitive to change.<br />

Increase in storm foredune<br />

damage and beach<br />

recession. The partially<br />

buried calcarenite<br />

topography could well lead<br />

to an indented coastline, of<br />

reefs and embayments.<br />

Foredune damage leads to<br />

dune de-stabilisation, and<br />

transport of sand across the<br />

barrier.<br />

2030: Occasional storm tide<br />

flooding above highest<br />

known tides.<br />

2070: Flooding will affect<br />

all swamps and adjacent<br />

low lying areas.<br />

Frequent storm damage to<br />

foredunes.<br />

(Impacts uncertain.<br />

Existing terrestrial<br />

vegetation is found in<br />

warmer conditions<br />

elsewhere)<br />

Dune vegetation adapts<br />

well to drier conditions, but<br />

recovers more slowly from<br />

fire, disease and storm<br />

damage: dune mobilization<br />

becomes more likely.<br />

Drains and creeks may<br />

increase sediment load to<br />

coastal swamps and lakes<br />

(this depends on land<br />

management practices).<br />

Aridity and sea level rise a<br />

threat to perched<br />

freshwater table within the<br />

Create a baseline for<br />

shoreline, dune and lake<br />

change by establishing a<br />

rectified aerial<br />

photographic record at an<br />

appropriate resolution.<br />

Maintain an aerial<br />

photographic record of<br />

shoreline change.<br />

Active management of<br />

dune blowouts.<br />

Manage sill height on tidal<br />

inlet to adjust to higher<br />

marine storm elevations<br />

as part of the adaptive<br />

management of Lake<br />

Bonney.<br />

Active management of<br />

dune blowouts.<br />

Active weed control<br />

within dunes.<br />

Maintain watching brief<br />

on sedimentation of Lake<br />

Bonney.<br />

Monitor salinity in small<br />

freshwater lakes. Adaptive<br />

management of plant<br />

Maintain<br />

connectivity of<br />

vegetation within<br />

the region.<br />

Limestone Coast and Coorong Coastal Action Plan 299

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