Current Advances in Coastal Wetland Elevation Dynamics: Introduction to the Special Issue DOI Creative Commons
Donald R. Cahoon, Glenn R. Guntenspergen

Estuaries and Coasts, Journal Year: 2024, Volume and Issue: 47(7), P. 1703 - 1707

Published: Aug. 2, 2024

The thematic issue entitled, "Current Advances in Coastal Wetland Elevation Dynamics," draws on topics from two special sessions at the CERF 2021 conference plus additional recent research describing scientific insights gained Surface Table–Marker Horizon (SET–MH) method and its application across globe to quantify understand subsurface process influences wetland elevation change responses sea-level rise. findings group articles within each of five topics. (1) A 30-year retrospective surface shallow dynamics. (2) Investigations soil elevation. (3) How community applies SET–MH RSLR other environmental drivers such as altered hydrology sediment supply. (4) data are used long-term monitoring networks different geographic scales. (5) Pairing SET-MH with (a) survey techniques increase lateral coverage trends (b) geodetic measurements vertical land motion.

Language: Английский

Measuring and Interpreting the Surface and Shallow Subsurface Process Influences on Coastal Wetland Elevation: A Review DOI
Donald R. Cahoon

Estuaries and Coasts, Journal Year: 2024, Volume and Issue: 47(7), P. 1708 - 1734

Published: April 2, 2024

Language: Английский

Citations

9

Linking tidal‐creek sediment fluxes to vertical sediment accretion in a restored salt marsh DOI Creative Commons
Daniel J. Nowacki, Jessica R. Lacy, S. La Selle

et al.

Earth Surface Processes and Landforms, Journal Year: 2025, Volume and Issue: 50(5)

Published: April 1, 2025

Summary Despite growing interest and investment in salt‐marsh restoration, relatively few marshes subjected to restoration efforts have been systematically monitored assess physical trajectory or success. In south San Francisco Bay, California, USA, where 83% of wetlands were lost via human manipulation, the largest wetland effort on US west coast is currently underway, restoring approximately 6000 ha former salt‐production ponds mixed habitats. The Whale Tail–Cargill Mitigation complex Bay has a century‐long history drainage, industrial use as subsequent recovery. Restoration 20 Cargill Marsh was initiated late 1990s when levee surrounding subsided, pond breached two locations, enabling conversion back habitat decades. Here, we present time‐series measurements sediment fluxes primary tidal creek entering complex, which are compared decadal‐scale sedimentation patterns determined from repeat elevation surveys cores collected at study site. All three methods show net import restored marsh. greatest equivalent rates occurred early with generally decreasing through time. long‐term average, expressed vertical rate, 1.8 cm year −1 . Rates data between 1.4 2.6 , higher earlier restoration. most recent estimates, computed instrument deployments, indicate seasonal variability import. Annualized lower winter, 0.1 summer, 1.7 Although our measured considerably greater than current local relative sea‐level rise (SLR) 0.3 an increase SLR decrease available suspended would threaten ability marsh keep pace avoid drowning future.

Language: Английский

Citations

0

Current Advances in Coastal Wetland Elevation Dynamics: Introduction to the Special Issue DOI Creative Commons
Donald R. Cahoon, Glenn R. Guntenspergen

Estuaries and Coasts, Journal Year: 2024, Volume and Issue: 47(7), P. 1703 - 1707

Published: Aug. 2, 2024

The thematic issue entitled, "Current Advances in Coastal Wetland Elevation Dynamics," draws on topics from two special sessions at the CERF 2021 conference plus additional recent research describing scientific insights gained Surface Table–Marker Horizon (SET–MH) method and its application across globe to quantify understand subsurface process influences wetland elevation change responses sea-level rise. findings group articles within each of five topics. (1) A 30-year retrospective surface shallow dynamics. (2) Investigations soil elevation. (3) How community applies SET–MH RSLR other environmental drivers such as altered hydrology sediment supply. (4) data are used long-term monitoring networks different geographic scales. (5) Pairing SET-MH with (a) survey techniques increase lateral coverage trends (b) geodetic measurements vertical land motion.

Language: Английский

Citations

0