Coral reefs are highly sensitive to prolonged periods of elevated seaβsurface temperature. When water temperatures exceed the normal seasonal maximum by roughly 1β―Β°C, the symbiotic algae (zooxanthellae) that provide corals with energy begin to expel, leading to the phenomenon known as coral bleaching.
To quantify this thermal stress, scientists use the DegreeβHeatingβWeeks (DHW) metric. DHW accumulates the temperature anomaly above a reference threshold (typically 1β―Β°C above the climatological maximum) for each week over a 12βweek window, providing a cumulative measure of heat exposure.
Higher DHW values correlate with increased bleaching risk and mortality. Management agencies employ DHW thresholds (e.g., 4β―Β°Cβweeks for moderate risk, 8β―Β°Cβweeks for severe risk) to trigger conservation actions such as reef monitoring and temporary fishing closures.
What is the Degree-Heating-Weeks (DHW) metric?
How does coral bleaching occur?
What is the reference threshold for coral bleaching?
How can I interpret the DHW values to assess bleaching risk?
What geographic areas are suitable for this calculator?
How often should I update the DHW values to monitor bleaching risk?
What are the long-term effects of coral bleaching?
Results are for informational purposes only and do not constitute professional advice.
