TY - JOUR
T1 - Projections of global delta land loss from sea‐level rise in the 21st century
AU - Nienhuis, Jaap H.
AU - Wal, Roderik
N1 - Funding Information:
We thank Sönke Dangendorf for sharing the RSLR reconstructions and Jorge Lorenzo‐Trueba for helpful conversations about sea‐level rise and deltas. We appreciate the constructive reviewing by Brad Murray and an anonymous reviewer, and editorial work from Kathleen Donohue. This research was supported by NSF award EAR‐1810855 and NWO award VI.Veni.192.123 to JHN and benefitted from the Water, Climate, Future Deltas program of Utrecht University.
Publisher Copyright:
© 2021. The Authors.
PY - 2021/7/28
Y1 - 2021/7/28
N2 - River deltas will likely experience significant land loss because of relative sea-level rise (RSLR), but predictions have not been tested against observations. Here, we use global data of RSLR and river sediment supply to build a model of delta response to RSLR for 6,402 deltas, representing 86% of global delta land. We validate this model against delta land area change observations from 1985–2015, and project future land area change for IPCC RSLR scenarios. For 2100, we find widely ranging delta scenarios, from +94 ± 125 (2 s.d.) km2 yr−1 for representative concentration pathway (RCP) 2.6 to −1,026 ± 281 km2 yr−1 for RCP8.5. River dams, subsidence, and sea-level rise have had a comparable influence on reduced delta growth over the past decades, but if we follow RCP8.5 to 2100, more than 85% of delta land loss will be caused by climate-change driven sea-level rise, resulting in a loss of ∼5% of global delta land.
AB - River deltas will likely experience significant land loss because of relative sea-level rise (RSLR), but predictions have not been tested against observations. Here, we use global data of RSLR and river sediment supply to build a model of delta response to RSLR for 6,402 deltas, representing 86% of global delta land. We validate this model against delta land area change observations from 1985–2015, and project future land area change for IPCC RSLR scenarios. For 2100, we find widely ranging delta scenarios, from +94 ± 125 (2 s.d.) km2 yr−1 for representative concentration pathway (RCP) 2.6 to −1,026 ± 281 km2 yr−1 for RCP8.5. River dams, subsidence, and sea-level rise have had a comparable influence on reduced delta growth over the past decades, but if we follow RCP8.5 to 2100, more than 85% of delta land loss will be caused by climate-change driven sea-level rise, resulting in a loss of ∼5% of global delta land.
KW - climate change
KW - land loss
KW - morphology
KW - river delta
KW - sea level rise
KW - sediment
UR - http://www.scopus.com/inward/record.url?scp=85111531501&partnerID=8YFLogxK
U2 - 10.1029/2021GL093368
DO - 10.1029/2021GL093368
M3 - Article
SN - 0094-8276
VL - 48
SP - 1
EP - 9
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 14
M1 - e2021GL093368
ER -