Model Prediction of Macroplastic Distributions in European Marine Basins: Comparison with Beach and Floating Macroplastic Observations and Estimation of Model Accuracy
Abstract
1. Introduction
2. Materials and Methods
2.1. The Lagrangian Model LTRANS
- The sources of macroplastics, which include both land sources and sea sources (maritime). Each macroplastic (or particle) is released at the surface at a specific time and location in each one of the basins. A detailed description is in Section 2.2.
- The 3D marine currents for each marine basin, which are computed with the General Estuarine Transport Model-GETM [17]. GETM is the hydrodynamic model within the JRC Blue2MF. The horizontal resolution of the GETM runs is specific for each basin: 4’ × 2’ for the Baltic Sea, 2’ × 2’ for the Black Sea, 5’ × 5’ for the Mediterranean Sea, and 5’ × 3’ for both the NWES and SWES basins. The atmospheric forcing datasets used as inputs in GETM are from the European Centre for Medium-Range Weather Forecasts (ECMWF-ERA5).
- The Stokes Drift fields also condition the marine macroplastics distributions [15,16]. For the runs in this study, the Stokes Drift fields used are downloaded from the Copernicus site (https://marine.copernicus.eu/). For our marine basins, they all are computed by wave models using the ECWMF-ERA5 surface winds. The Stokes Drift input files have finer resolution than the marine currents in each basin (Table S5), and the LTRANS runs include them averaged in the same horizontal grid as the marine currents. A detailed description is in Section S3.
- The bathymetry file of each marine basin, which is the same one used by the GETM hydrodynamic-model setup to compute the 3D marine currents.
2.2. The Sources of Macroplastics as Inputs in LTRANS Runs
2.2.1. Land-Based Macroplastic Inputs
- The LTRANS domain for the Mediterranean Sea does not include the Marmara Sea. For this reason, and given the direction of the currents at the Dardanelles Strait toward the Aegean Sea, we assume that the total amount of macroplastics released by the sources around the Marmara Sea is entering the Mediterranean Sea by the Strait of Dardanelles.
- Following the same rationale, the macroplastics released in the Azov Sea are entering the Black Sea via the Strait of Kerch.
2.2.2. Maritime-Based Macroplastic Inputs
2.3. Observations Available to Validate/Compare with the LTRANS Results
2.3.1. Observations of Macroplastics on the BEACHES
2.3.2. Observations of FLOATING Macroplastics at Open-Sea
2.4. Comparison of Model Results with the Available Data
2.4.1. Comparison of Model Results with Data on the BEACHES
- The EMODnet surveys included in the comparison (with survey periodicity lower or equal to 6 months) follow the general guidelines in [29,30,31]. Thus, once the litter items are counted and documented, they are removed from the beach, and no extra cleaning (e.g., by the local authorities) is carried out from that moment to the next EMODnet survey.
- The macroplastics in the EMODnet database have all arrived from the sea, and they were not dropped at the beach by beachgoers or other inland polluters.
- The beached time of the LTRANS macroplastics can vary from EMODnet survey to EMODnet survey and within the range of 1 day to the survey periodicity.
2.4.2. Comparison of Model Results with Data of FLOATING Macroplastics at Open-Sea
3. Results and Discussion
3.1. BEACHED Macroplastics: Comparison with Beach Observations and Estimation of Model Accuracy
3.1.1. Periodicity of the Beach Surveys in EMODnet Dataset
- Most of the beaches in all basins were surveyed approximately every 3 months. Some beaches were surveyed, following closely the guidelines in [29,30,31]. This is the case, for example, of the beaches in Spain in both the Mediterranean Sea and the SWES basin, and the Netherlands and Denmark in the NWES basin.
- Beaches with survey periodicities different from ~3 months are, for example, the Latvian beaches surveyed every 12 months, the Bulgarian beaches surveyed only once, the French beaches in the Mediterranean Sea with periodicity ~1 month, and the Italian beaches, where the main survey periodicities were quite variable and scattered around 4 and 8 months.
- The calendar months in which the surveys were carried out (Figure S2) indicate that, for some beaches, litter data for the Winter season were not collected: for example, the beaches of Sweden, Finland, Estonia, and Denmark. In contrast, the Summer is missing or almost missing for Greece, Croatia, and Cyprus, whereas for Latvia and Romania, data were only collected in the Summer.
3.1.2. Number of BEACHED LTRANS Macroplastics in the EMODnet Dates and Locations
- LTRANS would need more run-time to accumulate the observed EMODnet abundances.
- LTRANS input sources would not be releasing enough particles in the basin; it would indicate the lack of some sources of litter pollution in the model inputs.
- EMODnet abundances are too large because some litter items do not have a marine-origin. This is, some of the accounted EMODnet macroplastics included may have been produced elsewhere inland and accumulated directly from land to the beach.
- EMODnet abundances are too large because of the fragmentation of macroplastics into smaller pieces. Fragmentation and macroplastic sizes are not included in LTRANS.
3.2. FLOATING Macroplastics: Comparison with Floating Macroplastic Observations and Estimation of Model Accuracy
3.2.1. Mediterranean Sea: Comparison with MEDSEALITTER Observations
- The spatial accuracy of the LTRANS results may be better than the time accuracy.
- The correlation values between MEDSEALITTER and LTRANS densities indicate a time inaccuracy of ±2 days for LTRANS results.
- When we group/count the number of MEDSEALITTER observations according to the corresponding correlations with LTRANS, the histogram shows the maximum in correlation 0.7–0.8 with a Gaussian-like shape, except for a secondary peak in correlation 0.4–0.5 (Figure S8). The corresponding observations of that peak are mostly accumulated in the transect between Sicily and Sardinia (Figure 14), which is precisely one of the transects with many MEDSEALITTER observations available (Figure S4). It is, as well, the transect where the strip-width is mostly 50 m, instead of the more usual 100 m (Figure S9). If the strip-widths were 100 m, most densities of that transect (dark-red circles in Figure 12) would decrease and get closer values to LTRANS values (according to Equation S1 in Section S6 of the Supplementary Materials). The other transect from Sicily, going to/from Tunisia, also accumulates many observations (Figure S4) but has strip-widths of 100 m (Figure S9) and correlations larger than 0.6 (Figure 14).
- The geographical distribution of the MEDSEALITTER-LTRANS correlations overlaps the variability-map of the densities predicted by LTRANS in Figure 14. The variability is estimated with the standard deviation of the 3 years of LTRANS results, as a measure of the spread of the potential density values. We want to explore if the low values of MEDSEALITTER-LTRANS correlations may correspond to areas with large, predicted variability in the LTRANS density, meaning that the MEDSEALITTER observations at specific times may not be representative of the densities than LTRANS can calculate, if the number of macroplastics varies a lot with time in that area. In Figure 14, the low MEDSEALITTER-LTRANS correlations (dark-blue circles) are mostly distributed in areas with local higher variability estimated by LTRANS (darker-grey areas), mostly close to the coast. The exception is precisely the transects between Sicily and Sardinia, also mentioned in the previous paragraph.
3.2.2. Black Sea: Comparison with EMBLAS Observations
3.2.3. SWES Basin: Comparison with CleanAtlantic Data
4. Conclusions
- The comparison of BEACHED LTRANS predictions with EMODnet surveys indicates that the discrepancies between them are mainly located close to ports, river mouths, and coastal lagoons. The LTRANS input sources included may not be releasing enough particles in the basins.
- It could also indicate the lack of some point sources of macroplastic pollution in the model inputs.
- As well, the lower BEACHED LTRANS abundances with respect to the EMODnet observations may also be due to the potential inclusion of land-originated macroplastics that arrived directly from land at the beaches and accounted within the EMODnet surveys.
- The uneven sampling periodicity in many of the beach surveys available may also condition the comparison with the BEACHED LTRANS results.
- Comparing the FLOATING LTRANS results with the available observations indicates that the divergences between them may arise from the intrinsic characteristics of the floating macroplastic data collection at sea used for comparison, which depends on the ship’s availability: observations are available only at specific/scattered locations at sea and with time coordinates unevenly distributed in the time range of the study. On the other hand, in the future, the availability of extensive open-sea observations of floating macroplastics used to improve model inputs will help to increase the accuracy of the FLOATING LTRANS results. These observations would be collected within the frame of projects, such as MEDSEALITTER, that follow a precise protocol for data collection by ships, set up unique strip-width, and allow replicability by a predetermined route-based approach.
- The LTRANS assumption of a homogenous daily release of macroplastics within the month for each source may also condition the accuracy of the LTRANS predictions. Unfortunately, daily realistic input datasets per source location are not available at present.
- Not including fragmentation and sizes of the macroplastics in LTRANS may also contribute to the discrepancies of the model results with observations.
Supplementary Materials
Author Contributions
Funding
Data Availability Statement
Conflicts of Interest
Abbreviations
| AIS | Automatic Identification System |
| Blue2MF | Blue2 Modelling Framework |
| ECMWF | European Centre for Medium Range Weather Forecast |
| EMBLAS | Improving Environmental Monitoring in the Black Sea (I-II) Project |
| EU | European Union |
| EC | European Commission |
| EMODnet | The European Marine Observation and Data Network |
| EMODnet data | Data, surveys and files on beach litter collected, homogenised and distributed by EMODnet that was surveyed/monitored by the Member States to report to the MSFD. |
| GETM | General Estuarine Ocean Model |
| LTRANS | Lagrangian TRANSport model |
| MSFD | Marine Strategy Framework Directive |
| NOAA | National Oceanic and Atmospheric Administration |
| NWES | Atlantic North-West European Shelf |
| SWES | Atlantic South-West European Shelf |
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| Basin | Land-Based Macroplastic Inputs of LTRANS (Million Macroplastics/Year) |
|---|---|
| Baltic Sea | 64 |
| Black Sea | 86 |
| Mediterranean Sea | 377 |
| NWES | 135 |
| SWES | 53 |
| Basin | Fisheries-Related Macroplastic Inputs of LTRANS (Million Macroplastics/Year) |
|---|---|
| Baltic Sea | 1.2 |
| Black Sea | 4.4 |
| Mediterranean Sea | 30.7 |
| North-East Atlantic | 9.7 |
| Basin | Number of EMODnet Surveys with Periodicity ≤ 6 Months | % of EMODnet Surveys Used of Total Available |
|---|---|---|
| Baltic Sea | 669 | 91.6% |
| Black Sea | 24 | 100% |
| Mediterranean Sea | 501 | 72.9% |
| NWES | 135 | 99.3% |
| SWES | 111 | 100% |
| Basin | EMODnet and LTRANS CORRELATION | EMODnet and LTRANS CORRELATION [Min Values, MAX Values] | Horizontal Resolution km × km (Minute of Longitude × Minute of Latitude) |
|---|---|---|---|
| Baltic Sea | 0.77 [1 0.88] | 0.52 (Germany), 0.99 (Estonia) | 3 to 4.4 km (4’ × 2’) |
| Black Sea | 0.88 | 0.77 (Bulgaria), 0.99 (Romania) | 2.5 to 3.7 km (2’ × 2’) |
| Mediterranean Sea | 0.73 [2 0.74] | 0.51 (Greece), 0.99 (Malta) | 6.5 to 9.3 km (5’ × 5’) |
| NWES | 0.81 | 0.71 (Sweden), 0.99 (Netherlands) | 4 to 6.1 km (5’ × 3’) |
| SWES | 0.8 | 0.71 (Portugal), 0.87 (Spain) | 5.6 to 7.2 km (5’ × 3’) |
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Garcia-Gorriz, E.; Macias-Moy, D.; González-Fernández, D.; Arcangeli, A.; Ferreira-Cordeiro, N.; Duteil, O.; Miladinova, S.; Pärn, O.; Ruiz-Orejón, L.F.; Pasanisi, E.; et al. Model Prediction of Macroplastic Distributions in European Marine Basins: Comparison with Beach and Floating Macroplastic Observations and Estimation of Model Accuracy. Oceans 2026, 7, 26. https://doi.org/10.3390/oceans7020026
Garcia-Gorriz E, Macias-Moy D, González-Fernández D, Arcangeli A, Ferreira-Cordeiro N, Duteil O, Miladinova S, Pärn O, Ruiz-Orejón LF, Pasanisi E, et al. Model Prediction of Macroplastic Distributions in European Marine Basins: Comparison with Beach and Floating Macroplastic Observations and Estimation of Model Accuracy. Oceans. 2026; 7(2):26. https://doi.org/10.3390/oceans7020026
Chicago/Turabian StyleGarcia-Gorriz, Elisa, Diego Macias-Moy, Daniel González-Fernández, Antonella Arcangeli, Nuno Ferreira-Cordeiro, Olaf Duteil, Svetla Miladinova, Ove Pärn, Luis Francisco Ruiz-Orejón, Eugenia Pasanisi, and et al. 2026. "Model Prediction of Macroplastic Distributions in European Marine Basins: Comparison with Beach and Floating Macroplastic Observations and Estimation of Model Accuracy" Oceans 7, no. 2: 26. https://doi.org/10.3390/oceans7020026
APA StyleGarcia-Gorriz, E., Macias-Moy, D., González-Fernández, D., Arcangeli, A., Ferreira-Cordeiro, N., Duteil, O., Miladinova, S., Pärn, O., Ruiz-Orejón, L. F., Pasanisi, E., Crosti, R., & David, L. (2026). Model Prediction of Macroplastic Distributions in European Marine Basins: Comparison with Beach and Floating Macroplastic Observations and Estimation of Model Accuracy. Oceans, 7(2), 26. https://doi.org/10.3390/oceans7020026

