Coral Reefs: A Reef Resilience Toolkit Module

Mass Bleaching

Mass bleaching can be defined as events in which entire reef tracts or regions completely bleached. Photo @ Great Barrier Reef Marine Park Authority

Mass bleaching can be defined as events in which entire reef tracts, or regions, completely bleach. These events are primarily caused by elevated sea temperatures. Unfortunately, mass bleaching is becoming more common and widely distributed as we experience global climate change.

Favorable Bleaching Conditions

Whether a reef bleaches during “hot water” events depends on a variety of factors, but there are some basic predictors that scientists use. Typically, a temperature rise of 1-2°C above the long term average is enough to cause mass bleaching. However, whether an area bleaches, and the severity of bleaching, depends on the length of time the corals are exposed to elevated water temperatures. Higher temperatures can be destructive over a shorter period of time, while lower temperatures take longer to cause mass bleaching.

In addition to high temperatures, sunlight combines with heat to increase the impacts of temperature induced bleaching. Thus, when the water is warm, and the sky is clear of clouds, conditions are very favorable for bleaching. One of the physical factors that has been identified that likely increases resilience and resistance to bleaching is shading. When shade is present, either due to weather conditions or physical location of a coral, bleaching is less likely to occur.

Predicting Bleaching

Recently, scientists and managers have been developing tools to forecast bleaching events in various parts of the world. Because global weather patterns and sea surface temperatures are closely monitored, it is possible to predict with some accuracy when and where bleaching will occur. Using measures such as Degree Heating Weeks (DHW Methodology), scientists can monitor the duration of heat stress that particular geographies may be experiencing, using satellite technology. However, both local and regional factors difficult to monitor on a global scale continue to make highly accurate predictions difficult. At a minimum, information available through the Coral Reef Watch program can be used to raise awareness and ensure that managers are anticipating an event when conditions are favorable. Managers can sign up to receive automated email updates about reefs in their part of the world. Currently about 24 sites are being closely monitored in real time. For more information on being prepared for a bleaching event, see the section on Rapid Response in this toolkit.

Resources

A Reef Manager’s Guide to Coral Bleaching

Coral Reef Watch

 

See Full Citations

1 Marshall and Schuttenberg 2006

 

Bleaching Basics
Bleaching Biology
Mass Bleaching
Bleaching Impacts
Recovery from Bleaching
Ocean Acidification
Ocean Chemistry Essentials
Acidification Impacts
Management Strategies
Coral Disease
Causes
Impacts
Management
Identifying Resilience
Ecological Factors
Biological Factors
Physical Factors
Social Resilience
Principles
Strategies
Data Gathering
Data Collection
Data Analysis
Data Synthesis
GIS Example
Resilient MPA Design
Representation
Inclusion of Critical Areas
Incorporating Connectivity
Size and Spacing
Socioeconomic Criteria
Managing for Resilience
Implementing Resilience
Management Essentials
Bleaching Monitoring
Resilience Monitoring
Measuring Effectiveness
Broad-Scale Management
Communicating Resilience
Importance of Coral Reefs
Threats to Coral Reefs
Communication Tools
Communication Examples
Coral Restoration
Background
Physical Restoration
Biological Restoration
Coral Nurseries
Coral Transplantation
Monitoring and Maintenance
Restoration Case Studies
Case Studies
Agatti, India
Aldabra, Seychelles
Bonaire
British Virgin Islands
Florida Keys
Great Barrier Reef
Kimbe Bay, PNG
Kiunga, Kenya
Lesser Sunda Ecoregion
Maui, Hawai‘i
MesoAmerican Reef
Micronesia
Mozambique
Palau
Raja Ampat, Indonesia
U.S. Virgin Islands
Wakatobi, Indonesia
Resources
Glossary
References
Related Tools
www.reefresilience.org     Copyright © 2007-2012 The Nature Conservancy