Evidence guide

How Marine Heatwaves Are Defined

A warm anomaly becomes a marine heatwave only after it is compared with a location- and season-specific baseline and persists long enough to meet a stated event rule.

Reviewed 10 October 2026 · Sources accessed 10 October 2026

Event detection is a threshold calculation

A widely used framework defines a marine heatwave from daily temperature exceeding a seasonally varying 90th-percentile threshold for at least five consecutive days. The climatology period, temporal smoothing, spatial cell and treatment of short gaps must be recorded because they can change event boundaries.

Observation
Daily sea-surface or subsurface temperature with location and quality flags
Baseline
Seasonal climatology and percentile threshold calculated over a declared reference period
Event output
Start, end, duration, maximum intensity, cumulative intensity and category under the chosen method

Teaching threshold example

Day 1below
Day 2above
Day 3above
Day 4above
Day 5above
Day 6above

This diagram is editorial and contains no measured temperatures. Five consecutive “above” labels illustrate the event rule; they do not estimate an event at a real location.

Detection does not measure impact

A temperature event can be mapped from physical data, but bleaching, mortality, range shifts or fishery losses require biological observations matched in space and time. Species differ in acclimatization, life stage and exposure. A surface product may also miss subsurface refuges or heating.

Do not collapse these claims

  • Detected: the temperature series crosses the chosen threshold.
  • Attributed: models and counterfactual analysis assess how climate drivers changed event likelihood or intensity.
  • Impacted: ecological monitoring links exposure to a biological response while considering competing stressors.

Practice workflow

Use the Marine Heatwave Tracker to learn the interface, then replace its illustrative values with a documented dataset. Record product version, coordinates, depth, baseline dates, percentile, event rule and retrieval date before comparing locations.

Sources

Definitions and dataset documentation were checked on 10 October 2026. Threshold choices and product resolution must accompany any reported event.

Ocean field notebook / discoveries

Field plan: How Marine Heatwaves Are Defined

A warm anomaly becomes a marine heatwave only after it is compared with a location- and season-specific baseline and persists long enough to meet a stated event rule.

Station 01

System boundary

A threshold depends on the reference period and local seasonality, so duration, intensity and baseline must be read together. Relate that field focus to “Event detection is a threshold calculation” before moving to “Teaching threshold example.”

Station 02

Measurements to log

Pair field observations made with consistent sampling effort with regional records that expose spatial variation. Record depth, location, date, units and sampling effort so a change in conditions is not mistaken for a change in the ocean.

Station 03

Change signal

Compare “Teaching threshold example” with “Detection does not measure impact.” Decide whether the pattern represents exposure, response or recovery, and state the observation period needed to tell them apart.

Open the pre-dive checklist
  • Which variable can be observed directly?
  • Which mechanism needs a second instrument or comparison site?
  • What result from Hobday et al. (2016), a hierarchical approach to defining marine heatwaves and Hobday et al. (2018), categorizing and naming marine heatwaves would change the planned conclusion?