It is estimated that 33-50% of coral reefs worldwide have been largely or completely degraded (International Society for Reef Studies Consensus Statement, October 2015). Yet the data supporting these predictions are surprisingly sparse, and thereby their relation to the environment is unclear. The COral Reef Airborne Laboratory (CORAL) will pave the way to better predict the future of this global ecosystem and steward them through global change by addressing the question: What is the relationship between coral reef condition and biogeophysical forcing parameters? Over a three-year campaign, CORAL will:

Objective 1. Measure the condition of representative coral reefs across the global range of reef biogeophysical values. The primary indicators for coral reef condition are benthic cover (ratio of coral, algae, and sand), primary productivity, and calcification.

Objective 2. Establish empirical models that relate reef condition to biogeophysical forcing parameters. Ten primary biogeophysical parameters are selected for their recognized influence on components of the reef system, including:

  1. Coral species richness (biodiversity)
  2. Sea surface temperature
  3. Photosynthetically available radiation
  4. Aragonite saturation state
  5. Significant wave height
  1. Coastal development threat level
  2. Marine pollution threat level
  3. Overfishing threat level
  4. Watershed pollution threat level
  5. Integrated local threat level

CORAL covers the Mariana Islands, Palau, portions of the Great Barrier Reef, and the Main Hawaiian Islands. These regions cover wide ranges of reef type, physical forcing, human threats, and biodiversity.


Coral Scanner

CORAL will provide the most extensive and uniform picture to date of coral reef condition through the use of the Portable Remote Imaging Spectrometer (PRISM) instrument aboard the Tempus Applied Solutions Gulfstream-IV (G-IV) aircraft. PRISM will record the spectra of light reflected upward toward the instrument from the ocean below. Its very high spectral resolution is then used to identify reef composition (i.e., coral, algae, and sand) and model primary production. In situ data are obtained to validate the remote observations.


Coral Scanner


CL#16-2202

Site Manager: Sarah Lundeen

Webmaster: Sarah Lundeen