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Acoustic Surface Elevation Dynamics data Marconi salt marsh

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posted on 2022-01-10, 12:32 authored by Pim WillemsenPim Willemsen, Erik Horstman, T.J. (Tjeerd) Bouma, M. (Martin) Baptist, Marinka van PuijenbroekMarinka van Puijenbroek, B.W. (Bas) Borsje

At the semi-natural constructed Marconi salt marsh, bed level change data were collected using state-of-the-art Acoustic Surface Elevation Dynamics (A-SED) instruments. This recently developed instrument measures the distance between the bed and the instrument through the echo of an acoustic signal. The instrument is set-up to be able to collect measurements when the sensor of the instrument is fully inundated. A burst of eight samples (sampling frequency of 5 Hz) was stored at a measurement interval of 5 to 15 minutes. The instruments were installed downward looking, with the sensor head aimed vertically at the bottom. The instruments were serviced, cleaned and data were downloaded every two to three months. A post-processing script was developed in Python to convert the acoustic return signals to bed level change data. The measurements were validated with manual readings of the height above bed (HAB) of the sensors every time the instruments were serviced.


Funding

The Marconi field work was supported by the municipality of Delfzijl with funding from the Dutch Waddenfonds under grant number WF223001. Cash and in-kind co-funding was received from the consortium partners of EcoShape.

Mangrove-RESCUE: Mangrove Resilience for Enhanced Safety of Coastal Urbanisations and Environments

Dutch Research Council

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History

Publisher

4TU.ResearchData

Time coverage

September 2019 - September 2020

Geolocation

Delfzijl, the Netherlands

Geolocation Longitude

6.945025

Geolocation Latitude

53.327528

Format

zipped text files and python files

Organizations

Deltares; University of Twente; Faculty of Engineering Technology, Department of Water Engineering and Management; Wageningen University and Research, Wageningen Marine Research; Wageningen University and Research, Aquatic Ecology and Water Quality Management Group; Royal Netherlands Institute for Sea Research, Department of Estuarine and Delta Systems and Utrecht University