Viewers and Bulletins

Monitoring and forecasting Sargassum rely heavily on satellite observations, which allow scientists to detect surface accumulations and track their movement across the Atlantic. Modern sensors can identify Sargassum by its spectral signature and estimate its biomass over broad regions, providing monthly to weekly updates that support regional alerts.

Looking forward in time with short term predictions (up to 2-3 days approx.), not only the satellite observation of sargassum is needed but also fine scale representations of currents, tides, waves and wind to estimate how and where sargassum mat are pushed around. Yet satellites measurements are disturbed by clouds, cannot detect deeply submerged mats, or resolve small patches near the coast, which limits their capacity for short-term local predictions.

Numerical models are also used to offer tools to support short term to seasonal predictions.

As Sargassum approaches shore, its behavior becomes increasingly influenced by fine-scale winds, tides, waves, and coastal currents—processes that act at spatial scales too small for most satellites or basin-scale models to capture. To bridge this gap, forecasting systems are beginning to combine satellite data with high-resolution ocean models, particle-tracking simulations, and biological growth estimates that account for changing temperature, nutrients, and light. Ensemble methods and machine-learning approaches are also being tested to better predict strandings and provide early warnings. Despite these advances, substantial work is still needed to improve forecasting accuracy, especially in the final kilometers before landfall, where even small environmental changes can determine whether Sargassum reaches the shoreline or disperses offshore.

Monitoring

Copernicus Marine Service

Monitoring of Sargassum blooms across the tropical Atlantic, Caribbean Sea, and Gulf of Mexico shown 3 days before the day you open it. Violet dots indicate Sargassum mats detected by satellite, while the blue streamlines show surface currents. Together, they illustrate how ocean circulation drives the transport and accumulation of Sargassum. Note that some areas are not covered by space observations due to cloud cover or satellite’s trajectory.

Credit : Copernicus Marine Service

Space Climate Observatory

Sargassum location from SeSaM SCO project based on satellite-derived ocean color. To achieve the required accuracy—and thanks to extensive French‑American collaboration—it combines data of different resolutions, including Sentinel‑2 and Landsat 8 & 9 at 10 and 20 meters, Sentinel‑3 at 300 meters, and GOES at 1 kilometer. The latter has the advantage of being geostationary, providing images every 15 minutes, which helps overcome the issue of clouds, which are very common in the equatorial belt.

Credit : CLS

Forecasting

European Digital Twin Ocean

The European Digital Twin Ocean (EDITO) application Sargassum Forecast, currently in demonstration phase, provides forecasts of the seasonal distribution of sargassum in the North Atlantic up to six months. Produced by Mercator Ocean and based on real time detection and forecasting of sargassum developed under the project SeSaM, this application will integrate the European Union’s Digital Twin Ocean.

Bulletins and reports

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