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Wave conditions predicted mangrove presence at 400 coastal sites with 78.2% accuracy

A global study of 400 coastal sites found that periods of low wave energy help explain mangrove distribution, with a mechanistic model achieving 78.2% accuracy.

Illustrative coastal wetland and shoreline landscape with water, native plants and ocean waves

Why some coastlines support mangrove forests while others do not may depend heavily on how long the waves remain calm enough for young trees to establish. A new global study used 20 years of wave data at 400 coastal locations and achieved 78.2% accuracy in predicting whether mangroves were present.

Published in Nature on 30 September 2026, the research suggests that changing wave climates could alter the places where mangroves can survive, even when temperature and other environmental conditions appear suitable. The finding could reshape how conservation teams select sites for coastal restoration.

The authors did not simply identify a correlation between average wave height and forest cover. They developed a process-driven model built around windows of opportunity, periods when wave forcing falls low enough for seedlings to take hold. This distinction is central to understanding the study’s contribution.

What the study found

Mangrove forests are unusually important coastal habitats. They store carbon, provide nursery areas for aquatic life and help reduce some coastal hazards. Yet mangroves do not occupy every tropical and subtropical shoreline, including many locations where the broader climate seems suitable.

The researchers proposed that the early establishment stage helps explain this uneven distribution. Young seedlings face different challenges from mature trees. Even if an established forest can tolerate wave exposure, repeated disturbance may prevent a new generation of mangroves from becoming securely rooted.

Their model assessed the timing and intensity of wave forcing rather than relying on a single long-term average. Across 400 globally distributed coastal sites, it predicted mangrove presence or absence with an accuracy of 78.2%, according to the published study.

That result is useful, but it is not a guarantee that roughly four in five restoration projects would succeed. Classification accuracy describes how often the model matched observed site status within its evaluation framework. Actual planting success depends on many additional ecological and management factors.

How the researchers built the model

The study analysed two decades of open-source hindcast wave information, a type of reconstructed historical dataset derived from numerical modelling and available observations. It incorporated three swell partitions to represent wave energy arriving from different directions and systems.

The researchers used an effective wave-height measure that accounts for offshore wave conditions and the direction of waves relative to the coastline. A shore can be exposed to large offshore swells yet experience a different local impact depending on orientation and the angle of incoming waves.

The analysis included 400 coastal sites distributed across regions where mangroves occur. Locations without mangroves were selected from marine ecoregions containing mangrove forests, helping limit the possibility that broad climatic differences alone explained the contrast.

The model’s organising concept was the window of opportunity. Instead of asking only whether a location experiences strong waves, it examined whether sufficiently calm periods occur for seedlings to establish. A site with intermittent rough seas may still support mangroves if favourable intervals are long enough.

This process-based reasoning is more informative than treating every coastline with the same annual mean wave height as equivalent. Two sites can have similar averages but different sequences of storms, calm spells and wave directions, potentially producing different conditions for young plants.

Why calm periods matter

Mangrove establishment requires seedlings or propagules to arrive, remain in place and develop enough stability to withstand later disturbance. Wave energy can dislodge propagules, erode sediment or uproot fragile plants before they become established.

The sequence of events therefore matters. A severe wave event immediately after a propagule settles may prevent establishment, while the same event after roots have developed could have a different effect. The model attempts to capture this timing-dependent ecological bottleneck.

The researchers’ focus on open coasts also matters. Protected estuaries and sheltered lagoons experience different wave environments from exposed shorelines. Findings for the open coast should not automatically be applied to every mangrove habitat without further testing.

The study does not imply that waves are the only factor controlling mangrove distribution. Salinity, tidal inundation, sediment supply, propagule availability, coastal development and temperature remain relevant. Its contribution is to show that wave forcing can be a primary control that has been insufficiently represented in broad distribution models.

What 78.2% accuracy tells us

The headline accuracy indicates that the mechanistic model captured a substantial part of the observed distribution pattern across the evaluated locations. That lends support to the idea that opportunities for establishment are an important determinant of where open-coast mangroves persist.

However, accuracy alone does not reveal the model’s balance of false positives and false negatives. A false positive would identify a site as suitable for mangroves when none were observed. A false negative would classify an occupied site as unsuitable. Both matter for conservation planning.

The 400 locations also do not represent every possible coastline. Local conditions can vary sharply over short distances, especially where reefs, sandbars, coastal structures or complex shore geometry change the wave environment. Site-level assessment remains necessary.

It would also be misleading to describe the model as forecasting mangrove forest area or carbon storage with 78.2% accuracy. Its reported performance concerns the presence or absence of mangroves, a narrower outcome than predicting forest density, growth or the long-term services a restored habitat might provide.

Why this matters for restoration

Coastal restoration projects sometimes focus on whether the water, soil and climate appear suitable for mangroves. The new findings suggest that planners should also examine the frequency and duration of low-energy wave conditions, particularly during the early establishment period.

A site may look attractive during a calm inspection but be regularly disturbed before seedlings can root. Conversely, an exposed shoreline may still offer recurring intervals that permit establishment. Long-term wave records can reveal patterns that a single field visit misses.

The research could help identify where natural regeneration is plausible and where active interventions would face high physical risk. It could also inform the timing of planting or the design of measures intended to protect seedlings during their most vulnerable stage.

However, engineering a quieter shoreline is not automatically desirable. Breakwaters and other structures can alter sediment movement, nearby habitats and coastal processes. Restoration decisions should consider ecological trade-offs rather than treating wave reduction as an uncomplicated solution.

Climate change adds uncertainty

Changes in storm tracks, swell patterns and sea levels could alter the windows of opportunity available to mangrove seedlings. The study found that even modest shifts in wave forcing can affect modelled site suitability, implying that future distribution changes may occur without dramatic changes in average temperature.

This is particularly relevant because mangrove forests are often discussed as natural climate solutions. Protecting and restoring them can support carbon storage and coastal resilience, but the habitats themselves are exposed to changing physical conditions.

A location that currently supports establishment may become less favourable if calm periods shorten or disruptive waves become more frequent. Another site could become more suitable under a different regional wave regime. The direction of change will depend on local and regional conditions.

The model should not be interpreted as a precise forecast for every future shoreline. Projections depend on how wave conditions evolve and on ecological factors that were not fully captured. Long-term monitoring is needed to test whether predicted suitability changes translate into observed forest shifts.

What the study does not prove

The research provides evidence that wave conditions are important for mangrove presence, but it is not a global experiment in which wave exposure was manipulated independently. Its mechanistic design strengthens the ecological explanation, while observational distribution data still leave room for other influences.

The reported 78.2% accuracy also means that a meaningful share of locations were not classified correctly. That limitation should be viewed as an invitation to improve the model with finer-scale information rather than as a reason to dismiss the role of waves.

A presence-or-absence analysis does not measure forest health. A site with surviving mangroves may still be degraded, fragmented or unable to regenerate successfully. Conversely, a site without mangroves today might be suitable after other barriers, such as land conversion or restricted tidal flow, are addressed.

The study’s results are most directly relevant to wave-exposed open coasts. Applying them to sheltered estuaries, urban shorelines or highly engineered environments requires attention to the differences in hydrodynamics and the availability of propagules.

What comes next

Future research could combine the wave-based model with local measurements of sediment stability, propagule settlement, seedling survival and coastal development. Such work would help distinguish the physical barriers that can be managed from those that make restoration unlikely to succeed.

Testing the approach across restoration sites over several years would be especially valuable. Researchers could compare predicted windows of opportunity with actual seedling establishment and later survival, turning a promising distribution model into a more practical decision tool.

For policymakers, the message is that protecting mangroves requires more than identifying warm coastlines or counting planted trees. Understanding the physical conditions that allow forests to establish and regenerate may be just as important as safeguarding the trees that already exist.

The new study does not offer a universal recipe for restoration. It does, however, provide a quantified global demonstration that wave timing and exposure are central to the geography of mangrove forests, and that those conditions deserve a place in coastal climate adaptation planning.

Source Information

Study title: Global mangrove distribution on the open coast is controlled by waves.

Authors: Sarah Wells, Bradley Henderson, Andrew Dansie, Daniel A. Friess, Thorsten Balke and William Glamore.

Journal: Nature.

Publication date: 30 September 2026.

Study design: Global process-driven modelling of mangrove presence and absence using 20 years of hindcast wave data.

Sample: 400 globally distributed coastal sites.

Key result: 78.2% classification accuracy for observed mangrove presence or absence.

Original DOI: 10.1038/s41586-026-11089-z.

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