Coral Reefs: A Reef Resilience Toolkit Module

Causes of Mass Bleaching

Various sources of stress can cause individual corals to bleach. However, high water temperatures along with intense sunlight is the primary cause of mass bleaching events.

When coral reefs are exposed to warm water for sustained periods of time, large numbers of corals may bleach. A temperature increase of only 1-2°C above average hot season maximums can be sufficient to cause mass bleaching.

While high water temperature and bright sunlight are the primary triggers of mass bleaching, calm and clear conditions with minimal current can exacerbate the stress and intensify bleaching. Any factor that reduces these stressful conditions, such as cloud cover, strong winds, or tropical storms may be enough to protect the corals from bleaching.

Mass bleaching occurs when sea temperatures rise 1-2° C above normal summer maxima for an extended period and is accompanied by strong sunlight. Photo © Great Barrier Reef Marine Park Authority

Scientists believe that mass bleaching events have become more severe and widespread due to rising global temperatures linked to climate change.

When

In the warmest season, water temperatures are higher and bleaching is more likely. Warm seasons often coincide with calm conditions and the lack of wind and current results in less mixing, clearer seas, and deeper penetration of solar radiation, ultraviolet light, and photosynthetically active radiation (PAR).

Depending on the part of the world, mass bleaching can occur during El Niño years, for example, much of the Indian Ocean in 1998, and in others during La Niña years (e.g., Easter Island in 2000).1

Average global temperature has been rising. Bleaching has become more frequent and widespread over the past two decades. Predictions of continued warming seas cause concern that bleaching events will also continue to increase in frequency and intensity.

Resources

In Hot Water: Coral Bleaching Video Part 1

In Hot Water: Coral Bleaching Video Part 2

 

See Full Citations

1 Wellington et al. 2001

 

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