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Status of Caribbean coral reefs after bleaching and hurricanes in 2005

Status of Caribbean coral reefs after bleaching and hurricanes in 2005

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<strong>Status</strong> <strong>of</strong> <strong>Caribbean</strong> Coral Reefs <strong>after</strong> Bleach<strong>in</strong>g <strong>and</strong> Hurricanes <strong>in</strong> <strong>2005</strong>Recovery from hurricane damage is variable. Often, branch<strong>in</strong>g <strong>coral</strong>s recover quickly because<strong>of</strong> their rapid growth, <strong>and</strong> broken branches can even beg<strong>in</strong> to regrow <strong>in</strong> new areas. However,recovery can be h<strong>in</strong>dered by the accumulation <strong>and</strong> movement <strong>of</strong> <strong>coral</strong> rubble generated bythe hurricane, <strong>and</strong> by <strong>in</strong>creases <strong>in</strong> the abundance <strong>of</strong> algae, which compete for space with<strong>in</strong>the reef. Terrestrial run<strong>of</strong>f result<strong>in</strong>g from heavy ra<strong>in</strong>fall can also <strong>in</strong>fluence the nearshore reefecosystems, smother<strong>in</strong>g <strong>coral</strong>s with sediment <strong>and</strong> other debris, as well as <strong>in</strong>creas<strong>in</strong>g nutrients(<strong>in</strong>clud<strong>in</strong>g those <strong>in</strong> fertilisers) that <strong>in</strong>fluence growth rates <strong>of</strong> algae, <strong>and</strong> lower<strong>in</strong>g sal<strong>in</strong>ity,which can stress <strong>coral</strong>s.Co n c l u s i o n sThe <strong>in</strong>fluence <strong>of</strong> <strong>hurricanes</strong> on <strong>coral</strong> <strong>reefs</strong> can be beneficial <strong>and</strong> detrimental. Small <strong>hurricanes</strong>can provide fast relief dur<strong>in</strong>g periods <strong>of</strong> thermal stress, whereas waves from large <strong>hurricanes</strong>can reduce a reef to rubble. Coral <strong>reefs</strong> have experienced these effects <strong>of</strong> <strong>hurricanes</strong> <strong>and</strong>survived for millions <strong>of</strong> years; however, <strong>in</strong> light <strong>of</strong> the rapidly chang<strong>in</strong>g climate, the ability <strong>of</strong><strong>coral</strong>s to recover from severe storms, while fac<strong>in</strong>g the comb<strong>in</strong>ed effects <strong>of</strong> <strong>in</strong>creas<strong>in</strong>g thermalstress <strong>and</strong> ocean acidification, could be ext<strong>in</strong>guished.Ac k n o w l e d g e m e n t sInformation was extracted from the follow<strong>in</strong>g source <strong>and</strong> the authors would like to acknowledgetheir contribution: NOAA National Hurricane Center, www.nhc.noaa.govAu t h o r Co n ta c t sScott Heron, Jessica Morgan, Mark Eak<strong>in</strong> <strong>and</strong> William Skirv<strong>in</strong>g, NOAA Coral Reef Watch,SSMC1 Rm5308, 1335 East West Hwy, Silver Spr<strong>in</strong>g MD 20910, USA, scott.heron@noaa.gov,jessica.morgan@noaa.gov, mark.eak<strong>in</strong>@noaa.gov, <strong>and</strong> william.skirv<strong>in</strong>g@noaa.gov.References1. Manzello DP, Br<strong>and</strong>t M, Smith TB, Lirman D, Hendee JC, Nemeth RS (2007). Hurricanesbenefit bleached <strong>coral</strong>s. Proceed<strong>in</strong>gs <strong>of</strong> the National Academy <strong>of</strong> Sciences104:12035-12039.2. Massel SR, Done TJ (1993). Effects <strong>of</strong> cyclone waves on massive <strong>coral</strong> assemblages onthe Great Barrier Reef: meteorology, hydrodynamics <strong>and</strong> demography. Coral Reefs12:153-1663. Monaldo FM, Sikora TD, Bab<strong>in</strong> SM, Sterner RE (1997). Satellite Imagery <strong>of</strong> Sea SurfaceTemperature Cool<strong>in</strong>g <strong>in</strong> the Wake <strong>of</strong> Hurricane Edouard (1996). Monthly WeatherReview 125(10):2716–2721.4. Scharroo R, Smith WHF, Lillibridge JL (<strong>2005</strong>). Satellite Altimetry <strong>and</strong> the Intensification <strong>of</strong>Hurricane Katr<strong>in</strong>a. Eos Transactions 86:366.5. She<strong>in</strong> KA, Waple AM, Levy JM, Bourassa MA, et al. (2006). State <strong>of</strong> the Climate <strong>in</strong> <strong>2005</strong>.Bullet<strong>in</strong> <strong>of</strong> the American Meteorological Society 87(6):S1, 95 pgs.6. Trenberth KE, Shea DJ (2006). Atlantic <strong>hurricanes</strong> <strong>and</strong> natural variability <strong>in</strong> <strong>2005</strong>.Geophysical Research Letters 33:L12704.7. Webster PJ, Holl<strong>and</strong> GJ, Curry JA, Chang H-R (<strong>2005</strong>). Changes <strong>in</strong> Tropical Cyclone Number,Duration, <strong>and</strong> Intensity <strong>in</strong> a Warm<strong>in</strong>g Environment. Science 309:1844-1846.36

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