29.11.2014 Views

Cell Descriptions - South East Natural Resources Management Board

Cell Descriptions - South East Natural Resources Management Board

Cell Descriptions - South East Natural Resources Management Board

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

SE8 – Rivoli Bay<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 />

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 complex<br />

pattern of habitats sensitive<br />

to change.<br />

Increase in storm foredune<br />

damage and beach recession.<br />

Acceleration of erosional<br />

processes at <strong>South</strong>end and<br />

Beachport.<br />

Foredune damage leads to<br />

dune de-stabilisation, and<br />

transport of sand into and<br />

across the dune ridges.<br />

2030: Occasional storm tide<br />

flooding above highest<br />

known tides.<br />

2070: Flooding will affect all<br />

swamps and adjacent low<br />

lying areas.<br />

Frequent storm damage to<br />

foredunes.<br />

(Impacts uncertain. Existing<br />

terrestrial vegetation is<br />

found in warmer conditions<br />

elsewhere)<br />

Dune vegetation adapts to<br />

drier conditions, but<br />

recovers more slowly from<br />

fire and storm damage: dune<br />

mobilization becomes more<br />

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 />

Groundwater lowering a<br />

threat to Mullins Swamp,<br />

and dune ridge vegetation.<br />

Create a baseline for<br />

shoreline, dune and lake<br />

change by establishing a<br />

rectified aerial<br />

photographic record at<br />

an appropriate<br />

resolution.<br />

Maintain an aerial<br />

photographic record of<br />

shoreline change within<br />

Rivoli Bay.<br />

Use profiles to monitor<br />

these changes.<br />

Review sand budget<br />

within the whole bay.<br />

Active management of<br />

dune blowouts, where<br />

conservation values are<br />

threatened, as at Mullins<br />

Swamp.<br />

Manage valve on tidal<br />

inlet to adjust to higher<br />

marine storm elevations<br />

as part of the adaptive<br />

management of Lake<br />

Frome drain, and<br />

Mullins Swamp.<br />

Active management of<br />

dune blowouts.<br />

Active weed control<br />

within dunes.<br />

Maintain watching brief<br />

on sedimentation of<br />

Mullins Swamp.<br />

Monitor seasonal water<br />

levels and salinity in<br />

Mullins Swamp.<br />

Adaptive management<br />

Maintain<br />

connectivity of<br />

vegetation within<br />

the region.<br />

Limestone Coast and Coorong Coastal Action Plan 335

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!