Over the coming decades, a number of consequences of climate change are going
to be seen on reefs around the world. Exactly what is going to happen, we don't
know for sure. However, change is inevitable as the consequences of elevated
carbon dioxide into the atmosphere, including higher sea surface temperature and
ocean acidification, become more apparent.
For more information on this subject
AIMS
Marine Blueprint, "Climate Change and the Great Barrier Reef"
On this page, you can see some possible outcomes for parts of the Great
Barrier Reef of different climate change scenarios resulting from an increase in
sea surface temperature, taking into account the possible adaptability of coral.
It seems likely that the reefs will go on in some form, but it is possible
that they may host a different composition of species, depending on a range of
factors.
According to analysis by AIMS researcher Scott Wooldridge and co-authors (see
publication link, below), lasting transition to seaweed-dominated or otherwise
impoverished seascapes will be avoided only if there are slow rates of warming
and a significant rate of adaptation in corals.
Population levels of herbivorous creatures that live on the reef and keep it
clear of algae and seaweed will also play a part in how the reef might change.
Try selecting variables such as low or high warming, low or high rates of
adaptation, the location of the reefs and size of the herbivorous population to
see what might happen.
Try
the ReefState tool
| Please note:
Keep in mind when using this tool that it is indicative only, based upon
current knowledge and trends. These may change in the future as scientists
gain a better understanding of the potential (if any) for corals to adapt
to warmer ocean temperatures. The tool is also specific to particular
parts of the Great Barrier Reef and should not be taken as indicative of
possible trends for the whole GBR. It only deals with the threat posed by
predicted increases in the intensity of summer heat wave conditions and
does not take account of other ocean changes due to a changing climate,
including increasing acidification and changes in cyclone activity. For
those users who are interested in learning more about how the model was
developed and the assumptions upon which its predictions are based, please
refer to the paper by Scott Woodridge et al:
Precursors
for resilience in coral communities in a warming climate:
a belief network approach
(674kb PDF)
and
appendix (72kb PDF)
See
also how the Wooldridge et al paper has been cited by the
Intergovernmental Panel on Climate Change
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