TY - JOUR
T1 - Upstream and Downstream Boundary Conditions Control the Physical and Biological Development of River Deltas
AU - Piliouras, A.
AU - Kim, W.
N1 - Funding Information:
This project was supported by NSF EAR Grant 1324335 to W. Kim. Data are available through the SEAD data repository: 10.26009/s0YYHFYI (Low M) and 10.26009/s0QMHSQP (Runs 3b, High M). This research benefitted from useful conversations with Jim Buttles, Doug Jerolmack, and David Mohrig.
Funding Information:
This project was supported by NSF EAR Grant 1324335 to W. Kim. Data are available through the SEAD data repository: 10.26009/s0YYHFYI (Low M) and 10.26009/s0QMHSQP (Runs 3b, High M). This research benefitted from useful conversations with Jim Buttles, Doug Jerolmack, and David Mohrig.
Publisher Copyright:
©2019. American Geophysical Union. All Rights Reserved.
PY - 2019/10/28
Y1 - 2019/10/28
N2 - Relative sea level rise is depleting coastal land. Success in coastal restoration depends on understanding interactions between physical and biological processes that influence landscape change. We present results from flume experiments examining the coevolution of vegetation and delta channel networks. We show that channel mobility—controlled by upstream and downstream boundary conditions and delta size—controls vegetation colonization. The spatial patterns of plants in turn control the stability and spatial distribution of channels. Experiments with low-channel mobility develop large, dense plant patches that become denser over time and stabilize channels. Experiments with more mobile channels have sparse vegetation patterns that limit vegetation growth within existing patches, maintaining sparse, patchy vegetation. Thus, the ecogeomorphic development of deltas depends on the rate of channel lateral migration and avulsion, suggesting that upstream and downstream boundary conditions control both the physical and biological evolution of coastal landscapes.
AB - Relative sea level rise is depleting coastal land. Success in coastal restoration depends on understanding interactions between physical and biological processes that influence landscape change. We present results from flume experiments examining the coevolution of vegetation and delta channel networks. We show that channel mobility—controlled by upstream and downstream boundary conditions and delta size—controls vegetation colonization. The spatial patterns of plants in turn control the stability and spatial distribution of channels. Experiments with low-channel mobility develop large, dense plant patches that become denser over time and stabilize channels. Experiments with more mobile channels have sparse vegetation patterns that limit vegetation growth within existing patches, maintaining sparse, patchy vegetation. Thus, the ecogeomorphic development of deltas depends on the rate of channel lateral migration and avulsion, suggesting that upstream and downstream boundary conditions control both the physical and biological evolution of coastal landscapes.
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U2 - 10.1029/2019GL084045
DO - 10.1029/2019GL084045
M3 - Article
AN - SCOPUS:85074792638
SN - 0094-8276
VL - 46
SP - 11188
EP - 11196
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 20
ER -