Abstract:Human activities have increased nitrate export from rivers, degrading coastal water quality. At deltaic river mouths, the flow of water through wetlands increases nitrate removal, and the spatial organization of removal rates influences coastal water quality. To understand the spatial distribution of nitrate removal in a river‐dominated delta, we deployed 23 benthic chambers across ecogeomorphic zones with varying elevation, vegetation, and sediment properties in Wax Lake Delta (Louisiana, USA) in June 2018. R… Show more
“…2). Work in other systems has shown that network structure can also be used to estimate flux partitioning and the delivery of fluxes at the shore (Tejedor et al, 2015) and that estimation of nutrient and sediment fluxes can be addressed in similar ways (Dong et al, 2020;Knights et al, 2020).…”
Arising from the non-uniform dispersal of sediment and water that build deltaic landscapes, morphological change is a fundamental characteristic of river delta behavior. Thus, sustainable deltas require mobility of their channel networks and attendant shifts in landforms. Both behaviors can be misrepresented as degradation, particularly in context of the "stability" that is generally necessitated by human infrastructure and economies. Taking the Ganges-Brahmaputra-Meghna Delta as an example, contrary to public perception, this delta system appears to be sustainable at a system scale with high sediment delivery and long-term net gain in land area. However, many areas of the delta exhibit local dynamics and instability at the scale at which households and communities experience environmental change. Such local landscape "instability" is often cited as evidence that the delta is in decline, whereas much of this change simply reflects the morphodynamics typical of an energetic fluvial-delta system and do not provide an accurate reflection of overall system health. Here we argue that this disparity between unit-scale sustainability and local morphodynamic change may be typical of deltaic systems with well-developed distributary networks and strong spatial gradients in sediment supply and transport energy. Such non-uniformity and the important connections between network sub-units (i.e., fluvial, tidal, shelf) suggest that delta risk assessments must integrate local dynamics and sub-unit connections with unit-scale behaviors. Structure and dynamics of an integrated deltaic network control the dispersal of water, solids, and solutes to the delta sub-environment and thus the local to unit-scale sustainability of the system over time.
“…2). Work in other systems has shown that network structure can also be used to estimate flux partitioning and the delivery of fluxes at the shore (Tejedor et al, 2015) and that estimation of nutrient and sediment fluxes can be addressed in similar ways (Dong et al, 2020;Knights et al, 2020).…”
Arising from the non-uniform dispersal of sediment and water that build deltaic landscapes, morphological change is a fundamental characteristic of river delta behavior. Thus, sustainable deltas require mobility of their channel networks and attendant shifts in landforms. Both behaviors can be misrepresented as degradation, particularly in context of the "stability" that is generally necessitated by human infrastructure and economies. Taking the Ganges-Brahmaputra-Meghna Delta as an example, contrary to public perception, this delta system appears to be sustainable at a system scale with high sediment delivery and long-term net gain in land area. However, many areas of the delta exhibit local dynamics and instability at the scale at which households and communities experience environmental change. Such local landscape "instability" is often cited as evidence that the delta is in decline, whereas much of this change simply reflects the morphodynamics typical of an energetic fluvial-delta system and do not provide an accurate reflection of overall system health. Here we argue that this disparity between unit-scale sustainability and local morphodynamic change may be typical of deltaic systems with well-developed distributary networks and strong spatial gradients in sediment supply and transport energy. Such non-uniformity and the important connections between network sub-units (i.e., fluvial, tidal, shelf) suggest that delta risk assessments must integrate local dynamics and sub-unit connections with unit-scale behaviors. Structure and dynamics of an integrated deltaic network control the dispersal of water, solids, and solutes to the delta sub-environment and thus the local to unit-scale sustainability of the system over time.
“…10.1029/2020WR028090 2 of 14 and anthropogenic processes influence water, sediment, and nutrient transport pathways (Knights et al, 2020;Sanks et al, 2020). The USACE analyses (Fisk, 1952;Latimer & Schweitzer, 1951) were based on empirical analyses of extensive datasets.…”
Minor erosion measured in the Mississippi River would have reduced Atchafalaya Discharge, had Atchafalaya Basin remained constant. Lacustrine Deltas in the Atchafalaya Basin did not change partitioning, as they were downstream of a reach with steep water surface slope.
“…The development of the flow directions algorithms itself provided insights into the nature of river channel network structure in braided rivers and deltas (Schwenk et al, 2020). For deltas specifically, RivGr aph-extracted networks have been used to study how water and sediment are partitioned at bifurcations (Dong et al, 2020), to determine how distance to the channel network plays a controlling role on Arctic delta lake dynamics (Vulis et al, 2020), and to construct a networkbased model of nitrate removal across the Wax Lake Delta (Knights et al, 2020). For braided rivers, RivGraph was used to extract channel networks from hydrodynamic simulations in order to develop the novel "entropic braiding index" (eBI, Tejedor et al, 2019), and a function for computing the eBI (as well as the classic braiding index) for braided rivers is provided in RivGraph.…”
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