Climate change will likely have
significant impacts around the world. For instance, sea-level rise will compound
pressures that coastal communities already face, including erosion, storms,
and pressures from development. In arid and semi-arid regions, relatively
modest changes in precipitation can have large impacts on already limited
water supplies. Most projections of future impacts do not address what could
happen if warming continues beyond 2100, which is inevitable if steps to reduce
emissions are not taken, or if the rate of change accelerates. Even if greenhouse
gas emissions are reduced, some further warming is unavoidable, in that the
amount of CO2 released into the atmosphere in the next 30 years is expected
to double or triple. Global surface temperatures in 1999 set a new record
for the period of instrumental measurements, according to the NASA Goddard
Institute for Space Studies. The global temperature exceeded that of the previous
record year, 1995, by about 0.2°C (0.4°F). In the near term, agriculture
and forestry may benefit, but hotter and drier conditions increase the potential
for crop distributions to change. Areas around the world already having water
shortages or water quality problems will see these problems worsen.
In the latest report of IPCC's Working Group II, which addresses the vulnerability
of socio-economic and natural systems to climate change, scientists predict
glaciers and polar icecaps melting, countless species of animals, birds and
plant life dying out, farmland turning to desert, coral reefs destroyed, and
small island states submerged by the sea. The final report of Working Group
II addresses, among others issues:
The report addresses adaptation
options for each of these areas, and includes reports on regional concerns,
vulnerabilities and adaptive capacities in: Africa, Asia, Australia and New
Zealand, Europe, Latin America, North America, Polar Regions (Arctic and Antarctic)
and Small Island States. According to the report, “projected climate
changes during the 21st century have the potential to lead to future large-scale
and possibly irreversible changes in Earth systems, resulting in impacts on
continental and global scales.'' The Summary for Policymakers adds that "climate
change in polar regions is expected to be among the greatest of any region
on the Earth." Already, the extent and thickness of Arctic sea ice has
decreased, permafrost has thawed and the distribution and abundance of species
has been affected. The trends may continue even long after greenhouse gas
emissions are stabilized, causing irreversible impact on ice sheets, global
ocean circulation and sea levels.
The information presented above can be separated into biophysical
and socio-economic impacts. These are discussed briefly
below. This is not an exhaustive description of studies to date. Rather, it
is a brief outline of recent discussions on biophysical and socio-economic
impacts related to climate change. The aim is to promote discussion and encourage
knowledge sharing in relation to climate change impacts. It is hoped that
through this brief introduction, network users will be prompted to share their
reports, case studies and experiences in relation to biophysical and socio-economic
impacts of climate change at variable scales.
Principle Climate Drivers
and Associated Biophysical Impacts
There are several biophysical
impacts attributed to a changing climate. However, due to the limitations
of scientific knowledge in relation to predicted rates of climate change,
it is difficult to foresee impacts in quantifiable terms. Despite this, there
is general scientific consensus that the following biophysical impacts will
occur:
- Decline in species
diversity
- Changes in the hydrological
cycle
Projections on future
biodiversity levels show an overall decrease as a result of multiple pressures.
Because many of the impacts of biodiversity are occurring independent of climate
change, McCarthy et al (2001) suggest that the question becomes, ‘How
might climate change enhance or inhibit these loses in biodiversity?”
At present, there is limited evidence to suggest that climate change will
slow the loss of biodiversity; rather research indicates that increasing CO2
levels will favour invasive species and that increased nitrogen loads in the
biological cycle will reduce diversity of plants and animals. The projected
levels of diversity loss are variable relative to the climate change scenario
applied.
Principle Climate Drivers and Associated Socio-economic
Impacts
Human societies are, by nature, adaptable. Over centuries humans
have been adjusting to changes in their social and physical environments.
However, climate change poses a significant challenge for human societies.
The nature of climate change will see multiple alterations to social and ecological
environments. As a result, there are a number of socio-economic impacts that
are projected to occur (summarised in Table 1). These impacts have brought
adaptation, assessment and planning to the fore.
The geophysical response to climate change varies spatially and temporally.
Thus, Table 1 summarises general impacts against selected responses. Detailed
information on response-impact relations is available from the suggested links
and documents below.
Table 1:
Socio-economic Impacts of Geophysical Reponses to Climate Change
| Geophysical
Response to Climate Change |
Socio-economic
Impact |
| Warmer
climatic conditions |
- Increased
number of heat related illnesses in the elderly and poor
- Increased
energy demand, due to higher air conditioner use, increasing the risk
of blackouts
- Spread
of water borne, vector borne and food borne diseases
- Changes
in levels of agricultural production |
| Decline
in Rainfall |
- Changes
in agricultural production
- Increased
threat to urban water security
- Decline
in aquifer recharge |
| Increase
in Rainfall |
- Increased
flood, landslide, avalanche, and mudslide damage
- Increased
soil erosion
- Increased
recharge to floodplain aquifers |
| Increased
occurrence of extreme weather events |
- Numerous
problems for industry and infrastructure
- Societies
most at risk are those with high exposure to extreme climatic events
with limited adaptive capacity |
Principle Climate Drivers and
Associated Biophysical and Socio-Economic Coastal Impacts
In recent Intergovernmental Panel on Climate Change (IPCC)
assessments it has been emphasised that climate change brings with it other
implications for coasts, in addition to the threat of sea-level rise (Table
2). These climate change impacts include possible increases to sea-surface
temperatures, greater variability in the patterns of rainfall and runoff,
possible changes to wave climate, changes to the frequency, intensity and
duration of storms, and changes to ocean chemistry associated with global
warming, particularly ocean acidification. There is particular concern about
extreme weather events (floods, droughts and cyclones) that pose additional
threats to human infrastructure and settlements in the coastal zone. The tables
below provide a general summary of potential socio-economic impacts in global
coastal regions (Table 3) and the principle climate drivers and direct and
indirect impacts on the coast of Australia (Table 2).
Table 2.
Principal climate change drivers and possible direct and indirect impacts
on the coast of Australia, synthesised from IPCC and SURVAS summaries, with
tentative indication of confidence level in their likelihood of occurrence
(very high [VHC], high [HC], medium [MC], low [LC] or very low [VLC] confidence).
| Climate
Change (Driver) |
Principle
durect physical and ecosystem effects |
Potential
secondary and indirect impacts |
| Sea-level
change [VHC] (principally rise) |
Increased
coastal erosion [VHC]
Increased
inundation of coastal wetlands and lowlands [MC]
Increased
risk of flooding and storm damage [HC]
Increased
salinisation of surface and ground waters. [MC] |
Infrastructure
and economic activity impacted [MC]
Displacement
of vulnerable populations [LC] |
| Sea-surface
temperature [HC] (principally rise) |
Increased
coral bleaching [HC]
Pole
ward species migration [LC]
Increased
algal blooms [LC] |
Impact
on tourism [LC]
Possible
health impacts [LC] |
| Altered
precipitation and runoff [MC] (local increases/decreases) |
Altered
river sediment supply [MC]
Altered
lowland flood risk [MC]
Water
quality/nutrient impacts [LC] |
Implications
for erosion and flooding [LC] |
| Altered
wave climate [LC] (uncertain) |
Altered
wave run-up [VLC]
Altered
erosion and accretion [LC] |
Further
erosion [LC] |
| Storm frequency
and intensity changes [LC] (uncertain) |
Increased
waves and surges [LC]
Altered
cyclone zones [LC] |
Further
storm damage [LC] |
| Increases
in CO2 concentration in the atmosphere [VHC] and ocean [HC] |
Increased
ocean acidification [HC]
Increased
disruption to food chains (eg. Southern Ocean) [MC] |
Less
resilient reefs [LC]
Impaired
movement and function of high oxygen demand fauna (eg. squid, fish)
[MC] |
Table 3:
Socio-economic Impacts of Climate Change in Coastal Zones
| |
More Frequent
Floods |
Erosion
of coast |
Inundation
by sea water |
Increase
in water table |
Intusion
of salt water |
Change
in biological processes |
| Water resources |
|
|
√ |
√ |
√ |
√ |
| Agriculture |
√ |
|
√ |
√ |
√ |
|
| Human health |
√ |
|
√ |
|
|
√ |
| Fisheries |
√ |
√ |
√ |
|
√ |
√ |
| Tourism |
√ |
√ |
√ |
|
|
√ |
| Human settlements |
√ |
√ |
√ |
√ |
|
|
Source: UNFC
(2006)