L.M. Keyzer1*, J.D. Pietrzak1, P.M.J. Herman1,2, B.P. Smits2, R.K. James3, A.S. Candy, R.E.M. Riva1
Tropical shallow bays in the Caribbean, like Orient Bay and Galion Bay in Saint Martin, are often sheltered by coral reefs and covered with seagrass meadows. The ecosystems are linked through biological, chemical and physical processes. They provide valuable services such as habitat for many animals, tourism and coastal protection. But the system is threatened by climate change. Due to rising water temperatures and ocean acidification, coral reefs are not likely to keep up with sea-level rise. This will lead to a change in hydrodynamics, which might affect again the seagrass. This study focuses on how the change in hydrodynamics will impact the system. Due to the interdependency, the response of one of the elements might lead to a collapse of the entire system and the resulting loss of services. Shown is how the ecosystems stabilize the system and mitigate the impact of sea-level rise.
Within D-Flow FM a 2D depth-averaged hydrodynamic model has been set up for Orient Bay and Galion Bay, Saint Martin. The model is forced with the tide and average wind- and wave-conditions and includes vegetation. Using this model, the change in hydrodynamics due to 0.87 m sea-level rise is calculated. The dominant forcing is identified and the impact is related to the response of coral reefs to climate change. Next, the change in seagrass distribution is predicted using a statistical analysis. In this way it will be shown that ecosystems are able to mitigate the impact of sea-level rise.
A wave-driven circulation is found in the bays. The water depth above the reefs mainly determines the hydrodynamics inside the bays. Therefore, the change in hydrodynamics will depend on the response of coral reefs to climate change in general. When the reefs are able to keep up with sea-level rise, the change in hydrodynamics is limited. But in other cases, there will be a significant change in hydrodynamics. In Orient Bay, this will lead to a shift in the seagrass distribution. But on the scale of the entire bay, it is expected that the ecosystems are able to withstand the sea-level rise and valuable services are not lost. The key to conservation of the bays and its functions is preserving the reefs.
Figure 1 Change in RMS wave height [m]
Figure 2 Change in flow velocity [m/s]
Figure 3 Change in probability of seagrass occurrence [-]