Dataset Available

Dataset for: Revisiting salt marsh resilience to sea level rise: Are ponds responsible for permanent land loss?

Authors: Giulio Mariotti
Published On: Dec 16 2016 19:15 UTC
DOI: https://doi.org/10.7266/N7F769MX
UDI: R4.x264.196:0009
Files

Individual Files

No. of Downloads: 2

No. of Files: 8

File Size: 6.54 KB

File Format(s):
ASCII TXT (Matlab code)

Project Information

Funded By:
Gulf of Mexico Research Initiative

Funding Cycle:
RFP-IV

Research Group:
Coastal Waters Consortium II (CWC II)

Point of Contact

Jason Weick
Louisiana Universities Marine Consortium (LUMCON) / Data Management
jweick@lumcon.edu

Theme keywords

Marsh loss, Ponding, Wave erosion, RSLR thresholds, relative sea level rise

ISO 19115-2 Metadata
  View Metadata
Abstract:

A simple numerical model, written in Matlab, to simulate the long-term morphological evolution of marshes with ponds. The model is described in: Mariotti G. (2016) Revisiting salt marsh resilience to sea level rise: Are ponds responsible for permanent land loss? JGR-Earth Surface. 121(7): 1391-1407 DOI: 10.1002/2016JF003900

Suggested Citation:

Giulio Mariotti. 2016. Dataset for: Revisiting salt marsh resilience to sea level rise: Are ponds responsible for permanent land loss?. Distributed by: GRIIDC, Harte Research Institute, Texas A&M University–Corpus Christi. doi:10.7266/N7F769MX

Publications:

Mariotti, G. (2016). Revisiting salt marsh resilience to sea level rise: Are ponds responsible for permanent land loss? J. Geophys. Res. Earth Surf. doi:10.1002/2016jf003900

Purpose:

Predicting thresholds for salt marsh loss

Data Parameters and Units:

Rhos. inorganic sediment density. T. Tidal period. [s] tcr. Critical shear stress [Pa]; wind. Wind speed [m/s] amp. Tidal amplitude [m] range. Tidal range [m] (equal to 2 x amp) Be. Bank erodibility coefficient [m/yr] Bcreep. Creep coefficient [m/yr] Teta Bank slope [degrees] Slr. Relative sea level rise rate [mm/yr] Co. Reference sediment concentration [mg/l] Bmax. Maximum peak vegetation biomass [km/m2] nuGp. Rate at which organic matter is stored. [1/day] chiref. Fraction of refractory material [-] rhom. Dry bulk density of organic material [kg/m3] Dmin. Minimum elevation for vegetation growth with respect to MHW [m] Dmax. Maximum elevation for vegetation growth with respect to MHW [m] Temporary variables and derived parameters within the model: AA=0.25*(Dmin+Dmax)*(Dmax-3*Dmin) (see definition of Dmin and Dmax) depth= marsh depth relative to MHW [m] D=tidal average water depth Dep= rate of deposition [mm/s] totDEP total deposition = sum of organic and inorganic deposition balance= total deposition minus sea level rise rate s= vector of total net deposition as a function of depth needed to find the equilibrium depth dr= height of the marsh scarp PAR. Vector containing all the parameters

Individual Files: