TY - JOUR
T1 - Is “Morphodynamic Equilibrium” an oxymoron?
AU - Zhou, Zeng
AU - Coco, Giovanni
AU - Townend, IH
AU - Olabarrieta, Maitane
AU - van der Wegen, M.
AU - Gong, Zheng
AU - D’Alpaos, Andrea
AU - Gao, Shu
AU - Jaffe, Bruce
AU - Gelfenbaum, Guy
AU - He, Qing
AU - Wang, Yaping
AU - Lanzoni, Stefano
AU - Wang, Zhengbing
AU - Winterwerp, Han
AU - Zhang, Changkuan
PY - 2017/1
Y1 - 2017/1
N2 - Morphodynamic equilibrium is a widely adopted yet elusive concept in the field of geomorphology of coasts, rivers and estuaries. Based on the Exner equation, an expression of mass conservation of sediment, we distinguish three types of equilibrium defined as static and dynamic, of which two different types exist. Other expressions such as statistical and quasi-equilibrium which do not strictly satisfy the Exner conditions are also acknowledged for their practical use. The choice of a temporal scale is imperative to analyse the type of equilibrium. We discuss the difference between morphodynamic equilibrium in the "real world" (nature) and the "virtual world" (model). Modelling studies rely on simplifications of the real world and lead to understanding of process interactions. A variety of factors affect the use of virtual-world predictions in the real world (e.g., variability in environmental drivers and variability in the setting) so that the concept of morphodynamic equilibrium should be mathematically unequivocal in the virtual world and interpreted over the appropriate spatial and temporal scale in the real world. We draw examples from estuarine settings which are subject to various governing factors which broadly include hydrodynamics, sedimentology and landscape setting. Following the traditional "tide-wave-river" ternary diagram, we summarize studies todate that explore the "virtual world", discuss the type of equilibrium reached and how it relates to the real world.
AB - Morphodynamic equilibrium is a widely adopted yet elusive concept in the field of geomorphology of coasts, rivers and estuaries. Based on the Exner equation, an expression of mass conservation of sediment, we distinguish three types of equilibrium defined as static and dynamic, of which two different types exist. Other expressions such as statistical and quasi-equilibrium which do not strictly satisfy the Exner conditions are also acknowledged for their practical use. The choice of a temporal scale is imperative to analyse the type of equilibrium. We discuss the difference between morphodynamic equilibrium in the "real world" (nature) and the "virtual world" (model). Modelling studies rely on simplifications of the real world and lead to understanding of process interactions. A variety of factors affect the use of virtual-world predictions in the real world (e.g., variability in environmental drivers and variability in the setting) so that the concept of morphodynamic equilibrium should be mathematically unequivocal in the virtual world and interpreted over the appropriate spatial and temporal scale in the real world. We draw examples from estuarine settings which are subject to various governing factors which broadly include hydrodynamics, sedimentology and landscape setting. Following the traditional "tide-wave-river" ternary diagram, we summarize studies todate that explore the "virtual world", discuss the type of equilibrium reached and how it relates to the real world.
UR - http://10.1016/j.earscirev.2016.12.002
UR - http://resolver.tudelft.nl/uuid:dc6e2971-2d99-4741-89de-892a2687f242
M3 - Article
SN - 0012-8252
VL - 165
SP - 257
EP - 267
JO - Earth - Science Reviews
JF - Earth - Science Reviews
ER -