Abstract

Few datasets exist of high-frequency, in situ measurements of storm overwash, an essential mechanism for the subaerial maintenance of barrier islands and spits. Here we describe a new sensor platform for measuring bed-level change and estimating overwash inundation depths. Our MeOw (Measuring Overwash) stations consist of two ultrasonic distance sensors, a microprocessor board, and a camera and are capable of withstanding the impacts of large storm events, can be left unattended to collect data for months to years, and are relatively inexpensive. With the exception of the camera, the MeOw stations are built with all open-source hardware and software. Herein we provide complete instructions for manufacturing the MeOw stations and present observations from a single MeOw station for a three-month (2019) deployment on a frequently overwashed section of Smith Island, VA. The MeOw stations captured three large storm events over the course of the deployment (Hurricane Dorian, Tropical Storm Melissa, and a November nor’easter), as well as several high-tide events. Based on our interpretation of the raw data, bed-level changes occurred throughout the deployment from both storm and non-storm overwash, but were particularly large during Tropical Storm Melissa where initial accretion of approximately 0.15 m was followed by 0.77 m of erosion over three days. The maximum overwash inundation depth occurred during the nor’easter and measured approximately 0.83 m. The variability in bed level over the course of our experiment highlights the importance of in situ high frequency bed-level measurements for constraining overwash inundation depths. MeOw stations are ideally suited for measuring storm overwash — or any process that necessitates tracking bed and water level elevations at high frequency during harsh conditions.

Highlights

  • Overwash, the landward flow of water and sediment over a dune crest during highwater events, is an important process on sandy coastlines, and an essential mechanism for the subaerial maintenance of low-lying barrier systems

  • Our MeOw stations use two ultrasonic distance sensors — one housed within a monitoring well and the other mounted externally on MATERIALS AND METHODS The MeOw stations consist of two ultrasonic distance sensors, a cellular trail camera, and a data logger, all mounted to a PVC and metal structure

  • The MeOw stations are ideally suited for measuring storm overwash — or any process that necessitates tracking bed and water level elevations at high frequency during harsh conditions

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Summary

Introduction

The landward flow of water and sediment over a dune (or berm) crest during highwater events, is an important process on sandy coastlines, and an essential mechanism for the subaerial maintenance of low-lying barrier systems. The MeOw stations are weather resistant and, if securely mounted, can withstand high wind, energetic waves, sediment deposition and/ or erosion, and be left unattended for months to potentially years. Their ability to track the bed elevation at high frequency immediately before and after overwash events reduces uncertainty in water depth measurements, which is, for example, an important factor for calculating wave energy flux during overwash (e.g. Anarde et al 2020). We describe the development and construction of the MeOw stations, present data from extensive field testing, and discuss the limitations and considerations of this methodology

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