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Cell Descriptions - South East Natural Resources Management Board

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SE12 – Cape Jaffa<br />

Climate change<br />

element/ scenario<br />

Combined climate<br />

changes and sea<br />

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 />

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 pattern of<br />

dune habitats sensitive to<br />

change.<br />

Increase in beach recession,<br />

storm foredune damage and<br />

dune ridge instability. Loss of<br />

small cliff-backed pocket<br />

beaches.<br />

Foredune damage could lead<br />

to widespread dune destabilisation<br />

and transport of<br />

sand across dunes to the<br />

adjacent farmland.<br />

Shoreline recession in many<br />

places will continue as far as<br />

the calcarenite bluff at the<br />

back of the beach: thus, a<br />

change in the character of the<br />

shoreline, from narrow low<br />

energy beach to low cliffs.<br />

2030: Occasional storm tide<br />

flooding above highest known<br />

tides.<br />

2070: Frequent storm damage<br />

to foredunes.<br />

Create a baseline for<br />

shoreline, dune and<br />

lake change by<br />

establishing a rectified<br />

aerial photographic<br />

record at an<br />

appropriate resolution.<br />

Active management of<br />

dune blowouts.<br />

Maintain an aerial<br />

photographic record<br />

of change.<br />

Create buffer zone to<br />

allow dune retreat<br />

where feasible.<br />

Active management of<br />

dune blowouts.<br />

The creation of<br />

buffer zones to<br />

allow retreat of tide<br />

dependant<br />

ecosystems a<br />

regional issue with<br />

local implications.<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 />

(Impacts uncertain. Existing<br />

terrestrial vegetation is found<br />

in warmer conditions<br />

elsewhere)<br />

Maintain<br />

connectivity of<br />

vegetation within<br />

the region.<br />

Drier average<br />

conditions:<br />

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

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

Groundwater<br />

lowering; saline<br />

incursion:<br />

Nearshore sea<br />

Dune vegetation adapts to<br />

drier conditions, but recovers<br />

more slowly from fire and<br />

storm damage allowing weed<br />

colonisation, notably exotic<br />

grasses: dune mobilization<br />

becomes more likely.<br />

Groundwater lowering a threat<br />

to dune vegetation.<br />

Changes are unlikely to affect<br />

Active weed control<br />

within dunes.<br />

Adaptive management<br />

of ecological assets.<br />

Lowering of<br />

regional water table<br />

(and perched water<br />

tables in dunes) a<br />

threat to all habitats.<br />

Limestone Coast and Coorong Coastal Action Plan 417

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