Abstract
Coastal deltaic change is expected to be one of the major Earth-surface
hazards of the 21st century as deltas around the world face large
changes in sediment supply due to river damming, land-use changes and
climate change. We have combined estimates of present and future
sediment delivery and wave climates to predict the future morphologic
response of deltaic coastlines worldwide. Simple parameterizations and
key insights from coastline evolution models have allowed us to make
morphologic predictions around the globe for every delta on Earth. We
find that without human interference many deltas with decreased sediment
loads are expected to be reworked by waves into spits and barrier
islands. Other deltas are projected to experience increased sediment
flux, and, in some cases these growing deltas could transition from
wave-dominated to river-dominated morphologies. This unified, global
picture of future deltaic change will aid local management of deltaic
areas and also provide opportunities for inclusion of morphologic change
into Climate and Earth System Models.
Original language | English |
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Publication status | Published - 1 Feb 2016 |
Externally published | Yes |
Keywords
- 3022 Marine sediments: processes and transport
- MARINE GEOLOGY AND GEOPHYSICSDE: 3045 Seafloor morphology
- geology
- and geophysics
- MARINE GEOLOGY AND GEOPHYSICSDE: 4558 Sediment transport
- OCEANOGRAPHY: PHYSICAL