NSW Climate Impact Profile Interactive Map

Climate change is projected to affect different regions of NSW in different ways. The NSW Climate Impact Profile presents information on the likely impacts of climate change in each of the State Plan Regions.

For specific regional climate information, click on the region of interest on the map below.

HunterSydney/Central CoastNorth CoastNew England/North WestWestern NSWRiverina/MurraySouth EastIllawarra

Hunter

Changes in climate more details

Temperature iconTemperature

Virtually certain to rise. Average daily temperatures are likely to increase in all seasons, with greatest increases in spring and winter (by 2.0 to 3.0 °C).

Rainfall iconRainfall

Increases likely in all seasons except winter.


Physical responses more details

Sea Level iconSea Level

Virtually certain to rise. Sea level is projected to rise 0.4 m by 2050 and 0.9 m by 2100.

Run-off iconRun-off

Minor annual increases are likely because of substantial increases in summer run-off.

Fire iconFire

Fire regimes are likely to change, with increasing fire frequency more likely towards 2050.

Droughts iconDroughts

Short-term droughts are likely to become more severe. Medium- to long-term ones are likely to be less severe.

Floods iconFloods

Frequency is likely to increase because of rising sea levels and catchment-driven flooding.

Regional impacts more details

Land iconLand

The major coastline impact is likely to come from sea level rise. Erosion is likely to increase on the steeper slopes of the upper catchments. Coastal erosion will increase.

Settlements iconSettlements

Those near estuaries and beaches are likely to be the most vulnerable. Low-lying areas will flood more frequently.

Ecosystems iconEcosystems

The most vulnerable are those on foreshores, as well as highly cleared and fragmented forests and woodlands.

North Coast

Changes in climate more details

Temperature iconTemperature

Virtually certain to rise. Average daily temperatures are likely to increase in all seasons, with the greatest increases in winter (by 2.0 to 3.0 °C).

Rainfall iconRainfall

Will increase in summer and autumn and decrease in winter.

Physical responses more details

Sea Level iconSea Level

Virtually certain to rise. Sea level is projected to rise 0.4m by 2050 and 0.9m by 2100.

Run-off iconRun-off

Substantial increases in size and depth are likely in summer.

Fire iconFire

Fire regimes are likely to change, with increasing fire frequency likely towards 2050.

Droughts iconDroughts

Short-term droughts are likely to become more severe. Medium- to long-term ones are likely to be less severe.

Floods iconFloods

Rising sea levels and catchment-driven flooding are likely to increase flood frequency.

Regional impacts more details

Land iconLand

The major coastline impact is likely to be from sea level rise. Erosion is likely to increase on the steeper slopes of upper catchments.

Settlements iconSettlements

Sea level rise and the resulting erosion are likely to have substantial impacts on coastal settlements, beaches, public infrastructure and residential and commercial property.

Ecosystems iconEcosystems

Those vulnerable include saline wetlands, low-lying coastal ecosystems and fragmented forests in the hinterland.

Sydney/Central Coast

Changes in climate more details

Temperature iconTemperature

Virtually certain to rise. Average daily maximum and minimum temperatures are likely to increase in all seasons by 1.5 to 3.0 °C.

Rainfall iconRainfall

Likely to increase in all seasons except winter.


Physical responses more details

Sea Level iconSea Level

Virtually certain to rise. Sea level is projected to rise 0.4 m by 2050 and 0.9 m by 2100.

Run-off iconRun-off

Likely to increase substantially in summer.


Fire iconFire

Fire regimes are likely to change, with increasing fire frequency likely towards 2050.

Droughts iconDroughts

Short-term droughts are likely to become more severe. Medium- to long-term ones are likely to be less severe.

Floods iconFloods

Rising sea levels and catchment-driven flooding are likely to increase flood frequency.

Regional impacts more details

Land iconLand

Sea level rise and the resulting flooding and erosion will have major impacts on the coastline. Changes in rainfall are likely to increase sediment shedding from the hinterland.

Settlements iconSettlements

Those near estuaries and beaches are likely to be the most vulnerable. Low-lying areas will flood more frequently.

Ecosystems iconEcosystems

Low-lying coastal ecosystems are at risk, as are fragmented ecosystems such as those on the Cumberland Plain.

Illawarra

Changes in climate more details

Temperature iconTemperature

Virtually certain to rise. Minimum and maximum daily temperatures are likely to increase by 1.5 to 3.0 °C.

Rainfall iconRainfall

Likely to increase substantially in summer, with moderate increases in both spring and autumn.

Physical responses more details

Sea Level iconSea Level

Virtually certain to rise. Sea level is projected to rise 0.4 m by 2050 and 0.9 m by 2100.

Run-off iconRun-off

Likely to decrease moderately in spring but increase substantially in summer.

Fire iconFire

Fire regimes are likely to change, with increasing fire frequency likely towards 2050.

Droughts iconDroughts

Short-term droughts are likely to become more severe. Medium- to long-term ones are likely to be less severe.

Floods iconFloods

Rising sea levels and catchment-driven flooding are likely to increase flood frequency.

Regional impacts more details

Land iconLand

Sea level rise is likely to flood and erode parts of the coastline. Changes in rainfall will increase sediment shedding from the hinterland and erode banks.

Settlements iconSettlements

Those near estuaries and beaches are likely to be the most vulnerable to sea level rise and the resulting flooding and erosion.

Ecosystems iconEcosystems

The most vulnerable are those on foreshores and those that are highly cleared and fragmented, such as on the Illawarra coastal plain.

South East

Changes in climate more details

Temperature iconTemperature

Virtually certain to rise. Average daily maximum temperatures are likely to increase in all seasons, with the largest increases in autumn, winter and spring (by 2.0 to 3.0 °C).

Rainfall iconRainfall

Likely to increase in summer and decrease in winter. A reduction in snow cover is likely in alpine areas.

Physical responses more details

Sea Level iconSea Level

Virtually certain to rise. Sea level is projected to rise 0.4 m by 2050 and 0.9 m by 2100.

Run-off iconRun-off

Likely to decrease substantially in spring and increase substantially in summer.

Fire iconFire

Fire regimes are likely to change, with increasing fire frequency likely towards 2050.

Droughts iconDroughts

Short-term droughts are likely to become more severe. Medium- to long-term ones are likely to be less severe.

Floods iconFloods

Rising sea levels and catchment-driven flooding are likely to increase flood frequency and extent in the lower areas of coastal floodplains. More intense rainfall events will change flood behaviour everywhere else.

Regional impacts more details

Land iconLand

The major coastline impact is likely to be from sea-level rise. Dryland salinity is likely to increase because of changes in groundwater hydrology.

Settlements iconSettlements

Major impacts are likely from erosion and flooding. Low-lying settlements are particularly at risk.

Ecosystems iconEcosystems

Widespread changes in natural ecosystems are expected to occur, with snow-dependent ecosystems and alpine species at particular risk.

New England/North West

Changes in climate more details

Temperature iconTemperature

Virtually certain to rise. Average daily maximum and minimum temperatures will very likely increase by 1.0 to 3.0 °C.

Rainfall iconRainfall

Likely to increase in all seasons except winter.


Physical responses more details

Run-off iconRun-off

Yearly average is likely to increase as a result of substantial increases in summer run-off.

Fire iconFire

Fire regimes are likely to change, with increasing fire frequency likely towards 2050.

Droughts iconDroughts

Short-term droughts are likely to become more severe. Medium- to long-term ones are likely to be less severe.

Floods iconFloods

Increasing intensity of flood-producing rainfall events is likely to change flood behaviour.

Regional impacts more details

Land iconLand

Reductions in vegetation cover because of poorer growing conditions will leave some soils vulnerable to wind and water erosion.

Settlements iconSettlements

Increases in rainfall events are likely to increase flooding from urban streams and drainage systems.

Ecosystems iconEcosystems

High-altitude forests are likely to contract. Environmental stress placed on specialised biological communities will cause degradation.

Western NSW

Changes in climate more details

Temperature iconTemperature

Virtually certain to rise. Average daily minimum temperatures will very likely rise by 0.5 to
2.0 °C, depending on the season.

Rainfall iconRainfall

Likely to increase in summer and decrease in winter.

Physical responses more details

Run-off iconRun-off

Increases are likely in summer and autumn.


Fire iconFire

Fire regimes are likely to change, with increasing fire frequency likely towards 2050.

Droughts iconDroughts

Short-term droughts are likely to become more severe. Medium- to long-term ones are likely to be less severe.

Floods iconFloods

Increasing intensity of flood-producing rainfall events is likely to change flood behaviour. Soil moisture levels and water storage levels will affect the degree of change.

Regional impacts more details

Land iconLand

Erosion is likely to increase because of more frequent and intense storms and reduced vegetation cover. Vulnerable areas include some surface soils on the alluvial plains, and gullies on the slopes and plains.

Settlements iconSettlements

Flood-producing rainfall may increase flooding of property. This depends on catchment moisture levels and water storage levels at the time.

Ecosystems iconEcosystems

Hotter and drier conditions are likely to affect all natural ecosystems. The worst affected are likely to be riverine and wetland ecosystems.

Riverina/Murray

Changes in climate more details

Temperature iconTemperature

Virtually certain to rise. Average daily maximum temperatures will very likely be 1.5 to 3.0 °C higher in all seasons.

Rainfall iconRainfall

Likely to increase in summer and decline substantially in spring, autumn and winter.

Physical responses more details

Run-off iconRun-off

Minor annual decreases likely.


Fire iconFire

Fire regimes are likely to change, with increasing fire frequency likely towards 2050.

Droughts iconDroughts

Short-term droughts are likely to become more severe. Medium- to long-term ones are likely to be less severe.

Floods iconFloods

Increasing intensity of flood-producing rainfall events is likely to change flood behaviour. Soil moisture levels and water storage levels will affect the degree of change.

Regional impacts more details

Land iconLand

Reduced vegetation cover, caused by overall drier conditions, is likely to increase erosion risk. Areas vulnerable to erosion include the alluvial plains of the Riverina and gullies on the South West Slopes and Plains.

Settlements iconSettlements

There is likely to be a rise in the frequency and intensity of flood-producing rainfall that may increase flooding of property. This depends on catchment moisture levels and water storage levels at the time.

Ecosystems iconEcosystems

All are vulnerable. Wetlands are expected to suffer the largest declines in productivity and nutrient cycling.

Page last updated: 29 August 2011