Global sea levels are rising and increasing the risk to coastal communities from inundation and erosion.
The principal components contributing to global average sea level rise are the melting of land-based snow and ice reserves and the thermal expansion of the ocean water mass.
While global average sea level rise is relatively consistent, there are significant regional variations throughout the ocean basins of the world, which are attributable to:
- variations in the distribution of thermal expansion
- local and regional meteorological effects
- regional responses to modes of climate variability (for example, the El Nino-Southern Oscillation).
There is also considerable short and long-term variability in sea levels at any particular location, with this variability often extending over multiple decades.
There are two related measures of sea rise:
- absolute sea level rise, which is the increase in the ocean water level
- relative sea level rise, which is the increase in sea level recorded on land and is affected by land movement at the tide gauge site.
NSW Government policy
Following a review by the NSW Chief Scientist and Engineer (PDF 1.6 MB) and stage one coastal management reforms, the NSW Government announced that councils would have the flexibility to determine their own sea level rise projections to suit their local conditions. The Government would no longer prescribe statewide sea level rise projections for use by councils and the 2009 NSW Sea Level Rise Policy Statement would no longer be NSW Government policy.
The Office of Environment and Heritage has released guidelines on incorporating sea level rise into flood risk and coastal hazard assessment (PDF 1.8 MB).
These documents will be revised as part of the coastal reform process. In the interim, reference to the NSW sea level rise planning benchmarks in these documents should be taken as referring to council's adopted sea level rise projections. The government has recently announced the details on the stage 2 coastal management reforms, please see here for more details.
Recorded historical sea level rise
Recorded sea levels are influenced by factors such as tides, waves, storm surges, seasonal temperature effects, and longer term effects due to large-scale phenomena like the El Nino-Southern Oscillation. Therefore, short-term sea level records reflect short-term trends that may be different from long-term trends.
A 2011 analysis of global tide gauge records and satellite altimetry has found that:
- Global average sea levels increased by 210 mm from 1880 to 2009.
- While there was considerable variability in the rate of rise during the 20th century, there has been a statistically significant acceleration since 1900.
- Between 1993 and 2009, the estimated rate of rise was 3.2 ± 0.4 mm per year from the satellite altimetry data and 2.8. ± 0.8 mm per year from tidal records.
Longer term analysis of NSW data is available from tide records at Fort Denison based on relative sea level measurements (PDF 1.3 MB). Equipment to measure the influence of land movement on tide records at Fort Denison was installed in May 2012 and will provide improved estimates of absolute sea level rise at this site over time.
Further information on observed historical mean sea levels is available from:
- the Intergovernmental Panel on Climate Change (IPCC) fifth assessment report - Chapter 3 (PDF 47.1 MB)
- the CSIRO Centre for Marine and Atmospheric Research
- the Antarctic Climate and Ecosystems Cooperative Research Centre (ACE CRC) Report Card (PDF 2.2 MB)
- CSIRO and the Australian Bureau of Meteorology report: State of the Climate 2014
- Bureau of Meteorology Australian Baseline Sea Level Monitoring Project
Projected future sea level rise
The increase in global mean sea level over the last century is thought to be associated with global warming as a result of increasing greenhouse gas concentrations in the atmosphere. The IPCC concludes it is extremely likely that human influence has been the dominant cause of the observed warming since the mid-20th century and that future changes to climate are likely to depend on future greenhouse gas emissions.
In its fifth assessment report (2013), the IPCC has developed a range of future sea level rise projections associated with different greenhouse gas emission scenarios (representative concentration pathways (RCPs)). These indicate the following:
Likely global mean sea level rise range by 2100
(relative to 1986-2005)
Significantly Reduced Emissions (RCP 2.6)
Highest Emissions (RCP 8.5)
They also suggest the possibility of up to several tens of centimetres above these values if marine-based sectors of the Antarctic ice sheet collapse.
Beyond 2100, the IPCC concludes that it is virtually certain that global mean sea level will continue to rise for many centuries owing to thermal expansion of the oceans.
Data provided by the IPCC also indicate that sea level rise along the east coast of Australia might be 0% to 10% above the global average by 2100 (relative to 1986–2005), with higher rates offshore.
Further information on sea level rise projections is available from:
- the IPCC fifth assessment report - chapter 13 (PDF 32.0 MB)
Sea level rise and its impacts
Of all the impacts from climate change, the projected rise in mean sea level is a concern for management of the coastal zone in the longer term.
The potential implications of sea level rise over time include:
- Higher projected storm surge and inundation levels.
- Landward recession of sandy shorelines. Depending on the rate and scale of sea level rise, the environmental, social and economic consequences of recession within low lying inter-tidal areas, in particular, may be significant in the medium-long term.
- Salt water intrusion and landward advance of tidal limits within estuaries. This may have significant implications in the medium-long term for freshwater and saltwater ecosystems and development margins, particularly building structures and foundation systems within close proximity to the shoreline.
- Existing coastal gravity drainage, stormwater infrastructure and sewerage systems may become compromised over time as mean sea level rises.
- Sea level rise will influence the entrance opening regimes for intermittently closed and open lakes and lagoons (ICOLLs) and alter catchment flood behaviour over time.
- The level of protection provided by existing seawalls and other hard engineering structures will decrease over time due to the increasing threat from larger storm surges and inundation at higher projected water levels.
Coastal impacts research
Awareness of climate change impacts on the coastal zone is growing; however more work could be done on climate change impacts on the NSW coastline and estuaries.
OEH is undertaking research that takes an initial step towards addressing this knowledge gap. This work is outlined in the Coastal, Estuarine and Marine Environments - Knowledge Strategy 2013-17 and the Climate Change Impacts and Adaptation - Knowledge Strategy 2013-17 . This includes improving knowledge of the risks of coastal erosion and inundation to help coastal planners and communities make better decisions for land-use planning, asset protection and emergency response. The work includes analysis and modelling to deliver better understanding of the risks associated with sea level rise and extreme events, assessing how climate variability alters the risk of erosion, and determining how risks to infrastructure and habitat differ between estuaries.
OEH is also supporting coastal impact research to increase understanding of the climate risks and adaptation options through the NSW Adaptation Research Hub which is a collaboration between the NSW Government leading NSW research organisations. The Coastal Processes and Responses node is led by the Sydney Institute of Marine Science (SIMS) with support from the Australian Climate Change Adaptation Research Network for Settlements and Infrastructure (ACCARNSI). This node is focused on improving the knowledge base and information on coastal and estuary impact assessment, risk management and adaptation responses. It will inform management decisions and actions taken by local communities and councils in the coastal zone.
Historical and future impacts of East coast 'lows'
East coast 'lows' (ECLs) are amongst the most dangerous meteorological events affecting Australia, and certainly the most significant for coastal eastern Australia. They frequently have severe consequences in terms of flash flooding, wind damage, storm surge, and heavy and damaging seas. They are also responsible for heavy rainfall events that contribute significantly to total rainfall and runoff along the Australian East Coast.
The coarse resolution of the global climate models means they are currently unable to adequately model ECLs due to their relatively small spatial extent and short life span. Consequently, it is difficult to project how climate change will impact on this weather phenomenon.
OEH received $750,000 over three years from the Environmental Trust to better understand the historical and future impacts of East coast lows and other major weather patterns on the eastern seaboard.
A snapshot of future sea levels: photographing the king tide
More than 250 people joined in photographing our foreshores in January 2009 when NSW experienced a king tide. See these images and learn more about tides, sea levels and climate change.
The Office of Environment and Heritage (OEH) has had an overwhelmingly enthusiastic response to its request for people to assist in the photographic survey of the impact of the king tide which occurred on the morning of 12 January 2009. OEH has already received over two thousand images of the event within a week of the king tide. These photographs provide a statewide snapshot of areas currently vulnerable to tidal inundation will assist planning for future implications of sea level rise.
The king tide was predicted to peak in Sydney at 2.05 metres at Fort Denison, but on the day the peak recorded was only 1.96 metres. Although some 9 cm short of the predicted king tide, the water level reached was still a very high spring tide level. It is important to understand that local meteorological and weather effects can have a very significant impact on water levels with variances of 20 cm not uncommon compared to the tide predictions. The fair weather and the presence of a high pressure system across most of coastal NSW at the time were the primary reasons for the tide level not reaching the predicted maximum.
OEH would like to thank all those who volunteered their time and photographed the king tide.
For more information please contact Team Leader Coastal Unit on (02) 4904 2590 or by email email@example.com.
For more information
NSW Coastal planning approaches
For additional technical information "Fort Denison Sea Level Rise Vulnerability Study" (PDF 1.26MB)