Map showing the paths that ocean current-following surface drifters deployed in coral larval slicks off west Maui traveled in 24 hours following their release during a coral spawning event. Such data suggests that the coral reefs off west-central Maui may provide coral larvae to the reefs off northeastern Lānaʻi.
Coral reefs are facing increasing stress from climate change (elevated sea-surface temperatures and acidification), combined with local stresses from over-fishing and sedimentation and other sources of land-based pollution. In light of the potential for these stressors to increase the rate of coral reef degradation to epidemic levels, coral reef scientists and managers world-wide are shifting emphasis towards identifying the key mechanisms controlling reef resiliency. There is a compelling need for information that will help managers identify processes and specific areas, at the jurisdictional level, where coral reefs will be the most viable in the future and where, given the unpredictability of stresses, reefs might be best suited for recovery. For example, some coral reefs that had been decimated by bleaching in 1997–1998 subsequently made rapid recoveries; clearly, identifying reefs having such potential will be powerful management tool in this era of increasing stress agents. This shift by the scientific community from identifying the processes of decline to identifying solutions for the future is highlighted in many recent publications, workshops, and international meetings.
Underwater photograph of coral (Montipora capitata) egg-sperm bundles floating to the surface during a coral spawning experiment off west-central Maui. Photograph by Eric Brown, National Park Service.
Much of the thinking thus far by the scientific community has focused on the biologic indicators of resiliency, such as coral cover, species diversity, and fish populations. The parameters that influence the health and sustainability of coral reefs are diverse and include changes in watersheds, coastal development, stream discharge, coastal circulation, and larval pathways and natural causes of stress (for example, large wave events in Hawaiʻi). They also include potential natural processes that reduce stress (for example, upwelling, internal-wave mixing, submarine groundwater discharge). Identifying areas of coral reefs that have the highest potential for survival requires a cross-cutting assessment of all of the salient geographic, geologic, and oceanographic factors as well.
Very little effort thus far has addressed potential reef managed/protected areas using a comprehensive evaluation of all the important processes that affect the health and long-term viability of a reef. Understanding the variability in mechanisms underlying resilience is critical for reef management under climate change, for reefs able to rapidly recover due to a combination of resiliency factors may serve as key refugia, or sources of larvae, for reef recovery at larger scales.
Map showing the location of existing marine managed/protected areas in the Maui Nui complex in the Hawaiian islands, which encompasses the islands of Molokaʻi, Maui, Lānaʻi, and Kahoʻolawe. [larger version]
This effort represents a new level of research and coordination, and we will have a two-fold approach.
The approach to these interdisciplinary studies will rely on a combination of laboratory efforts, field measurements and physics-based numerical monitoring. We use a wide range of tools to try to answer these questions, including: oceanographic instruments (for example, acoustic Doppler current profilers, wave/tide gauges, temperature sensors, salinity sensors, turbidity sensors, chemical sensors) mounted on the seabed or on moorings, water-column profilers with similar suites of sensors, GPS-equipped Lagrangian surface drifters, drop and towed underwater video mapping systems, swath acoustic mapping systems, airborne and space-based remote sensing imagery, and physics-based numerical models.
Prouty, N.G, Yates, K.K., Smiley, N., Gallagher, C., and Storlazzi, C.D., 2018, Carbonate system parameters of an algal-dominated reef along west Maui: Biogeosciences, doi: 10.5194/bg-2018-35.
Storlazzi, C.D., Gingerich, S.B., van Dongeren, A., Cheriton, O.M., Swarzenski, P.W., Quataert, E., Voss, C.I., Field, D.W., Annamalai, H., Piniak, G.A., and McCall, R., 2018, Most atolls will be uninhabitable by the mid-21st century because of sea-level rise exacerbating wave-driven flooding: Science Advances, v. 4 no. 4, doi: 10.1126/sciadv.aap9741.
Bahr, K.D., Jokiel, P.L., and Toonen, R.J., 2015, The unnatural history of Kāneʻohe Bay: coral reef resilience in the face of centureis of anthropogenic impacts: PeerJ, v. 3, n. e950, doi: 10.7717/peerj.950.
Ferrario, F., Beck, M.W., Storlazzi, C.D., Micheli, F., Shepard, C.C., and Airoldi, L., 2014, The effectiveness of coral reefs for coastal hazard risk reduction and adaptation: Nature Communications, 5:3794, doi:10.1038/ncomms4794.
Ganguli, P.M., Swarzenski, P.W., Dulaiova, H., Glenn, C.R., and Flegal, A.R., 2014, Mercury dynamics in a coastal aquifer: Manualua Bay, Oʻahu, Hawaiʻi: Estuarine, Coastal and Shelf Science, v. 140, p. 52-65, doi: 10.1016/j.ecss.2014.01.012.
Jokiel, P.L., Jury, C.P., and Kuffner, I.B., 2016, Coral calcification and ocean acidification, in, Hubbard, D.K., Rogers, C.S., Lipps, J.H., and Stanley, J., G.D., Eds., Coral Reefs at the Crossroads Vol. 6, New York, NY, Springer, pp. 7–45, doi: 10.1007/978-94-017-7567-0_2.
Quataert, E., Storlazzi, D., van Rooijen, A., Cheriton, O., van Dongeren, A., 2015, The influence of coral reefs and climate change on wave-driven flooding of tropical coastlines: Geophysical Research Letters, doi: 10.1002/015GL064861.
Storlazzi, C.D., Brown, E.K., and Field, M.E., 2006, The application of acoustic Doppler current profilers to measure the timing and patterns of coral larval dispersal, Coral Reefs, v. 25, no. 3, p. 369-381, doi: 10.1007/s00338-006-0121-x.
Storlazzi, C.D., Cheriton, O.M., Lescinski, J.M.R., and Logan, J.B., 2014, Coastal circulation and water-column properties in the War in the Pacific National Historical Park, Guam—Measurements and modeling of waves, currents, temperature, salinity, and turbidity, April–August 2012: U.S. Geological Survey Open-File Report 2014-1130, 104 p.
Presto, M.K., Storlazzi, C.D., Logan, J.B., Reiss, T.E., and Rosenberger, K.J., 2012, Coastal circulation and potential coral-larval dispersal in Maunalua Bay, Oʻahu, Hawaii—Measurements of waves, currents, temperature, and salinity, June–September 2010: U.S. Geological Survey Open-File Report 2012-1040, 67 p.
U.S. Geological Survey, 2009, Science-based strategies for sustaining coral ecosystems: U.S. Geological Survey Fact Sheet 2009-3089, 4 p.
Field, M.E., Cochran, S.A., Logan, J.B., and Storlazzi, C.D., 2008, The Molokaʻi coral reef today, and alternatives for the future, in Field, M.E., Cochran, S.A., Logan, J.B., and Storlazzi, C.D., eds., The coral reef of south Molokaʻi, Hawaiʻi; Portrait of a sediment-threatened fringing reef, U.S. Geological Survey Scientific Investigations Report, 2007-5101, p. 167-170.
Field, M.E., Cochran, S.A., Logan, J.B., and Storlazzi, C.D., eds., 2008, The coral reef of south Molokaʻi, Hawaiʻi; Portrait of a sediment-threatened reef, U.S. Geological Survey Scientific Investigations Report, 2007-5101, 180 p.
Field, M.E., Berg, C.J., and Cochran, S.A., 2007, Science and management in the Hanalei watershed; a trans-disciplinary approach: U.S. Geological Survey Open-File Report 2007-1219, 87 p.
Hatcher, G.A., Reiss, T.E., and Storlazzi, C.D., 2004, Application of GPS drifters to track Hawaiian coral spawning: U.S. Geological Survey Open File Report 2004-1309, p. 14.