Abstract
River sediments play a critical role in sustaining deltaic wetlands. Therefore, concerns are raised about wetlands’ fate due to the decline of river sediment supply to many deltas. However, the dynamics and drivers of suspended sediment near deltaic coasts are not comprehensively assessed, and its response to river sediment supply changes remains unclear. Here we examine patterns of coastal suspended sediment concentration (SSC) and river sediment plume area (RPA) for 349 deltas worldwide using satellite images from 2000 to 2020. We find a global increase in SSC and RPA, averaging +0.46% and +0.48% yr−1, respectively, with over 59.0% of deltas exhibiting an increase in both SSC and RPA. SSC and RPA increases are prevalent across all continents, except for Asia. The relationship between river sediment supply and coastal SSCs varies between deltas, with as much as 45.2% of the deltas showing opposing trends between river sediments and coastal SSCs. This is likely because of the impacts of tides, waves, salinity, and delta morphology. Our observed increase in SSCs near river delta paints a rare promising picture for wetland resilience against sea-level rise, yet whether this increase will persist remains uncertain.
| Original language | English |
|---|---|
| Article number | 3319 |
| Number of pages | 12 |
| Journal | Nature Communications |
| Volume | 15 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 18 Apr 2024 |
Bibliographical note
Publisher Copyright:© The Author(s) 2024.
Funding
We thank the NASA LP DAAC for providing MODIS SR data and GEE for providing image processing resources. We also thank Dr. Murray for providing the wetland area change data and Dr. Dethier for providing the river sediment flux data. L.F.,\u00A0X.H.,\u00A0and F.S. were supported by the National Natural Science Foundation of China (Nos: 42321004,\u00A042301392,\u00A0and\u00A042271348). X.H. was supported by the Fundamental Research Funds for the Central Universities, Sun Yat-Sen University (NO: 23qnpy08). J.N. was supported by the National Science Foundation (EAR-GLD-1810855) and the Dutch Research Council (VENI.192.123).
| Funders | Funder number |
|---|---|
| NASA LP DAAC | |
| Fundamental Research Funds for the Central Universities | |
| National Science Foundation | EAR-GLD-1810855 |
| Sun Yat-Sen University | 23qnpy08 |
| Nederlandse Organisatie voor Wetenschappelijk Onderzoek | VENI.192.123 |
| National Natural Science Foundation of China | 42301392, 42321004, 42271348 |
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