Multi-scale variability of storm Ophelia 2017: The importance of synchronised environmental variables in coastal impact

Emilia Guisado-Pintado; Derek W T Jackson

doi:10.1016/j.scitotenv.2018.02.188

Multi-scale variability of storm Ophelia 2017: The importance of synchronised environmental variables in coastal impact

Sci Total Environ. 2018 Jul 15:630:287-301. doi: 10.1016/j.scitotenv.2018.02.188. Epub 2018 Feb 23.

Authors

Emilia Guisado-Pintado¹, Derek W T Jackson²

Affiliations

¹ Department of Physical Geography and Regional Geographic Analysis, University of Seville, Seville 41004, Spain; School of Geography and Environmental Sciences, Ulster University, Coleraine, BT5241SA, Northern Ireland, United Kingdom. Electronic address: eguisado@us.es.
² School of Geography and Environmental Sciences, Ulster University, Coleraine, BT5241SA, Northern Ireland, United Kingdom. Electronic address: d.jackson@ulster.ac.uk.

PMID: 29477826
DOI: 10.1016/j.scitotenv.2018.02.188

Abstract

Low frequency, high magnitude storm events can dramatically alter coastlines, helping to relocate large volumes of sediments and changing the configuration of landforms. Increases in the number of intense cyclones occurring in the Northern Hemisphere since the 1970s is evident with more northward tracking patterns developing. This brings added potential risk to coastal environments and infrastructure in northwest Europe and therefore understanding how these high-energy storms impact sandy coasts in particular is important for future management. This study highlights the evolution of Storm (formally Hurricane) Ophelia in October 2017 as it passed up and along the western seaboard of Ireland. The largest ever recorded Hurricane to form in the eastern Atlantic, we describe, using a range of environmental measurements and wave modelling, its track and intensity over its duration whilst over Ireland. The impact on a stretch of sandy coast in NW Ireland during Storm Ophelia, when the winds were at their peak, is examined using terrestrial laser scanning surveys pre- and post-storm to describe local changes of intertidal and dune edge dynamics. During maximum wind conditions (>35 knots) waves no >2m were recorded with an oblique to parallel orientation and coincident with medium to low tide (around 0.8m). Therefore, we demonstrate that anticipated widespread coastal erosion and damage may not always unfold as predicted. In fact, around 6000m³ of net erosion occurred along the 420m stretch of coastline with maximum differences in beach topographic changes of 0.8m. The majority of the sediment redistribution occurred within the intertidal and lower beach zone with some limited dune trimming in the southern section (10% of the total erosion). Asynchronous high water (tide levels), localised offshore winds as well as coastline orientation relative to the storm winds and waves plays a significant role in reducing coastal erosional impact.

Keywords: Beach; Dune toe; Erosion; Hurricane; Terrestrial laser scanner; Wave run-up.