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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><strong>and</strong> current satellite images, complemented by direct measures like temperature loggers <strong>and</strong>buoys, were used to warn <strong>of</strong> the impend<strong>in</strong>g <strong>bleach<strong>in</strong>g</strong> threat. The products were distributedwidely through e-mail alerts <strong>and</strong> various <strong>in</strong>ternet sites, alert<strong>in</strong>g natural resource managers <strong>of</strong>the potential for damage to their <strong>coral</strong> <strong>reefs</strong>. Hundreds <strong>of</strong> scientists <strong>and</strong> resource managers <strong>in</strong>the <strong>Caribbean</strong> used these alerts <strong>and</strong> products <strong>in</strong> <strong>2005</strong> to allocate large amounts <strong>of</strong> their limitedf<strong>in</strong>ancial <strong>and</strong> logistic resources to monitor what turned out to be a record-break<strong>in</strong>g <strong>bleach<strong>in</strong>g</strong>event. The <strong>in</strong>formation yielded from this monitor<strong>in</strong>g will be vital to future management effortsto protect <strong>coral</strong> <strong>reefs</strong> <strong>in</strong> light <strong>of</strong> today’s rapidly chang<strong>in</strong>g climate.Th e <strong>2005</strong> Co r a l Bl e a c h i n g Ev e n t a n d Hu r r i ca n e sThese follow<strong>in</strong>g HotSpot images <strong>and</strong> the other ‘Degree Heat<strong>in</strong>g Week’ images on the front cover<strong>and</strong> <strong>in</strong>side title page are typical <strong>of</strong> the <strong>in</strong>formation that was widely dispersed throughout the<strong>Caribbean</strong> <strong>and</strong> elsewhere via the Internet through the <strong>coral</strong> reef <strong>in</strong>formation network ‘Coral-List’. This generated considerable correspondence, <strong>and</strong> senior NOAA scientists have <strong>of</strong>feredtheir personal <strong>in</strong>sight <strong>of</strong> what happened <strong>in</strong> their <strong>of</strong>fices as the sequence <strong>of</strong> events developed.These are detailed <strong>in</strong> Chapter 4.This 1st figure illustrates a typical HotSpot image (explanation on p. 38) that was generated fromsatellite data <strong>and</strong> distributed throughout the Wider <strong>Caribbean</strong>. The HotSpot on 16 July <strong>2005</strong> showswaters 1ºC to 2ºC above the normal summer maximum as seen as ‘warm’ yellow <strong>and</strong> orange colorsover central America as well as a large but less warm region <strong>in</strong> the central Atlantic Ocean; as this wasbe<strong>in</strong>g reported there was evidence <strong>of</strong> <strong>bleach<strong>in</strong>g</strong> reported <strong>in</strong> Belize.The first signs <strong>of</strong> <strong>bleach<strong>in</strong>g</strong> were <strong>in</strong> Brazil <strong>in</strong> March dur<strong>in</strong>g the southern summer. However,this did not correspond to a major HotSpot; it was more likely due to a local calm weather <strong>and</strong>heat<strong>in</strong>g event. The first <strong>coral</strong> <strong>bleach<strong>in</strong>g</strong> <strong>in</strong> the <strong>Caribbean</strong> was reported <strong>in</strong> early June on theIslas del Rosario <strong>in</strong> northwest Colombia where waters had warmed to 30 o C. These waters thencooled <strong>and</strong> the <strong>coral</strong>s recovered. By late June, surface waters exceeded 30 o C around Puerto8

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