Abstract

Light detection and ranging (Lidar) derived digital elevation models are widely used in modeling coastal marsh systems. However, the topographic error in these models can affect simulations of marsh coverage and characteristics. We investigated the relevance and impact of this error in micro- and mesotidal systems. Lidar-derived and RTK-adjusted topography were each used in a dynamic marsh model, and the resulting marsh coverages were examined. For two microtidal sites (Apalachicola, FL, USA, and Grand Bay, MS, USA) using solely lidar-derived topography, the model produced Cohen Kappa values of 0.1 for both estuaries when compared with National Wetland Inventory data indicating “very poor agreement.” Applying the RTK-adjusted topography improved the model marsh coverage results to “substantial agreement” with the values to 0.6 and 0.77, respectively. The mesotidal site in Plum Island, MA, USA, contained similar topographic errors, but the model produced a Cohen Kappa value of 0.73, which categorized it as “very good agreement” with no need for a further topographic adjustment given its present robust biomass productivity. The results demonstrate that marsh models are sensitive to topographic errors when the errors are comparable to the tidal range. The particular sensitivity of the modeling results to topographic error in microtidal systems highlights the need for close scrutiny of lidar-derived topography.

Highlights

  • S ALT marshes are responsible for positive impacts on coastal ecosystems, including wave energy attenuation, shorelineManuscript received April 18, 2019; revised January 30, 2020; accepted February 9, 2020

  • Comparisons of the elevations in the digital elevation models (DEMs) and the RTK measurements confirm the positive bias in lidar-derived DEMs

  • RTK data from marsh platforms in two microtidal and one mesotidal estuaries were compared with lidar-derived DEMs

Read more

Summary

Introduction

S ALT marshes are responsible for positive impacts on coastal ecosystems, including wave energy attenuation, shorelineManuscript received April 18, 2019; revised January 30, 2020; accepted February 9, 2020. By trapping sediment and increasing the elevation of the marsh platform, marshes can adapt to water-level changes and associated effects, such as erosion and increased inundation from tides and storm surge. This mechanism is enhanced with greater vegetation density, biomass production, and marsh coverage [10]. Due to the many services provided by marshes and their dynamic response to SLR, there has been an effort to create models that predict marsh coverage and evolution These models aim to present actionable information for mitigating marsh loss or to provide restoration planning and coastal management guidance [14]

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call