Coral reefs worldwide, and the services they provide, are seriously threatened by anthropogenic climate change and its impacts, including ocean
acidification and coral bleaching. Here, we present global projections for these key coral reef threats. The projections are based on
ensembles of the IPCC Fifth Assessment Report
(AR5) climate models using experiments with selected
Representative Concentration Pathways (RCPs)
.
All projections presented within
van
Hooidonk et al. (2014) are shown in a Google Earth file (a kmz file,
~1.2MB). We encourage all viewers to read the Contents
Description found at the 'About this product' page at the top of the file
directory structure containing the images (see "My Places" in the left-hand side
of the Google Earth interface).
The methods and names of the models used in the projections can be found here.
Problems viewing the file are likely to have one of three causes: 1) you need to clear everything from your 'My Places' folder or need to de-select anything saved there; 2) you need to download the most current version of Google Earth; and/or 3) the limitations of your PC or graphics card don't allow for the file to be viewed.
This research was made possible by a grant from the
Pacific
Islands Climate Change Cooperative to the authors of
van
Hooidonk et al. (2014)
.
Any information used from these projections should be cited as 'van Hooidonk et al. (2014)'. Image screen captures from the Google Earth file should always appear with 'adapted from van Hooidonk et al. (2014)', if used in presentations, reports, publications, web pages, etc. For questions about the projections and methods, please email the lead author, Ruben van Hooidonk, at ruben.van.hooidonk@noaa.gov. |
van
Hooidonk R, Maynard J, Manzello D, Planes S (2014)
van
Hooidonk R, Maynard J, Planes S (2013)
References
Opposite latitudinal
gradients in projected ocean acidification and bleaching impacts on coral reefs.
Global Change Biology, doi: 10.1111/gcb.12394.
Temporary refugia for coral reefs in a warming world.
Nature Climate Change, 3, 508-511, doi: 10.1038/nclimate1829.