TY - JOUR
T1 - Seaward expansion of salt marshes maintains morphological self-similarity of tidal channel networks
AU - Yang, Zicheng
AU - Finotello, Alvise
AU - Goodwin, Guillaume
AU - Gao, Chao
AU - Mudd, Simon
AU - Lague, Dimitri
AU - Schwarz, Christian
AU - Tian, Bo
AU - Ghinassi, Massimiliano
AU - D'Alpaos, Andrea
N1 - Funding Information:
This work was supported by the University of Padova SID2016 project titled “From channels to rock record: morphodynamic evolution of tidal meanders and related sedimentary products” (grant BIRD 168939 to Massimiliano Ghinassi), by the project HYDROSEM (Progetti di Eccellenza CARIPARO 2017, Cassa di Risparmio di Padova e Rovigo): “Fluvial and tidal meanders of the Venetian-Po plain: From hydrodynamics to stratigraphy” (PI Massimiliano Ghinassi), by the University of Padova Supporting TAlent in ReSearch (STARS) Grant entitled “TiDyLLy - Tidal network dynamics as drivers for ecomorphodynamics of low-lying coastal regions” (PI Alvise Finotello), and by the University of Padova SID2021 project “Unraveling Carbon Sequestration Potential by Salt-Marsh Ecosystems” (P.I. A. D'Alpaos). Z.Y. would like to thank the Fondazione Cariparo, for providing the essential funding for his Ph.D. study. Z.Y. also thanks Dr. Zeng Zhou for discussions regarding channel network evolution. We are grateful for constructive reviews from anonymous reviewers and the associate editor, which helped improve this paper.
Publisher Copyright:
© 2022 Elsevier B.V.
PY - 2022/11/12
Y1 - 2022/11/12
N2 - Tidal channel networks (TCNs) dissect ecologically and economically valuable salt marsh ecosystems. These networks evolve in response to complex interactions between hydrological, sedimentological, and ecological processes that act in tidal landscapes. Thus, improving current knowledge of the evolution of salt-marsh TCNs is critical to providing a better understanding of bio-morphodynamic processes in coastal environments. Existing studies of coastal TCNs have typically focussed on marshes with either laterally stable or eroding edges, and suggested that TCN morphology evolves primarily through the progressive landward erosion of channel tips, that is, via channel headward growth. In this study, we analyze for the first time the morphological evolution of TCNs found within salt marshes that are characterized by active lateral expansion along their seaward edges and anthropogenically-fixed landward boundaries. We use remote-sensing and numerical-modeling analyses to show that marsh seaward expansion effectively limits headward channel growth and prompts the evolution of TCNs that maintain self-similar morphological structures. In particular, we demonstrate that the overall TCN length increases proportionally to the rate at which marshes expand laterally and that these morphological changes do not significantly alter the drainage properties of the coupled marsh-TCN system. Such behavior is not observed in marshes that are not expanding laterally. Our results allow for elucidating the mechanisms of TCN formation and evolution in tidal wetlands, and are therefore critical to improving our current understanding of coastal-landscape ecomorphodynamics, as well as to developing sustainable strategies for the conservation and restoration of these environments.
AB - Tidal channel networks (TCNs) dissect ecologically and economically valuable salt marsh ecosystems. These networks evolve in response to complex interactions between hydrological, sedimentological, and ecological processes that act in tidal landscapes. Thus, improving current knowledge of the evolution of salt-marsh TCNs is critical to providing a better understanding of bio-morphodynamic processes in coastal environments. Existing studies of coastal TCNs have typically focussed on marshes with either laterally stable or eroding edges, and suggested that TCN morphology evolves primarily through the progressive landward erosion of channel tips, that is, via channel headward growth. In this study, we analyze for the first time the morphological evolution of TCNs found within salt marshes that are characterized by active lateral expansion along their seaward edges and anthropogenically-fixed landward boundaries. We use remote-sensing and numerical-modeling analyses to show that marsh seaward expansion effectively limits headward channel growth and prompts the evolution of TCNs that maintain self-similar morphological structures. In particular, we demonstrate that the overall TCN length increases proportionally to the rate at which marshes expand laterally and that these morphological changes do not significantly alter the drainage properties of the coupled marsh-TCN system. Such behavior is not observed in marshes that are not expanding laterally. Our results allow for elucidating the mechanisms of TCN formation and evolution in tidal wetlands, and are therefore critical to improving our current understanding of coastal-landscape ecomorphodynamics, as well as to developing sustainable strategies for the conservation and restoration of these environments.
U2 - 10.1016/j.jhydrol.2022.128733
DO - 10.1016/j.jhydrol.2022.128733
M3 - Article
VL - 615 Part A.
JO - Journal of Hydrology
JF - Journal of Hydrology
SN - 0022-1694
M1 - 128733
ER -