Peter Ganderton

ORCID: 0000-0003-4550-319X
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About
Contact & Profiles
Research Areas
  • Coastal and Marine Dynamics
  • Ocean Waves and Remote Sensing
  • Geological formations and processes
  • Coral and Marine Ecosystems Studies
  • Marine and fisheries research
  • Coastal wetland ecosystem dynamics
  • Oceanographic and Atmospheric Processes
  • Peatlands and Wetlands Ecology
  • Marine and coastal plant biology
  • Geophysics and Gravity Measurements
  • Soil erosion and sediment transport
  • Flood Risk Assessment and Management
  • Aquatic and Environmental Studies
  • Underwater Acoustics Research
  • Aerodynamics and Fluid Dynamics Research
  • Aeolian processes and effects

University of Plymouth
2002-2023

As global temperatures continue to rise, shallow coral reef bleaching has become more intense and widespread. Mesophotic ecosystems reside in deeper (30-150 m), cooler water were thought offer a refuge shallow-water reefs. Studies now show that mesophotic instead have limited connectivity with corals but host diverse endemic communities. Given their extensive distribution high biodiversity, understanding susceptibility warming oceans is imperative. In this multidisciplinary study of an atoll...

10.1038/s41467-023-42279-2 article EN cc-by Nature Communications 2023-10-16

Abstract Aim Research on mesophotic coral ecosystems (MCEs) has increased exponentially in recent decades, and the significance of this ecosystem been recognised both terms biodiversity distribution. However, research mostly focussed corals is globally sporadic, with Indian Ocean remaining largely unexplored overall MCEs under protected. Hence, baseline data MCE benthic communities lacking, but nonetheless essential for developing adequate management strategies. Here, we assess variation...

10.1111/ddi.13777 article EN cc-by Diversity and Distributions 2023-10-04

Manning, A.J.; Martens, C.; De Mulder, T.; Vanlede, J.; Winterwerp, J. Ganderton, P. and Graham G. W., 2007. Mud Floc Observations in the Turbidity Maximum Zone of Scheldt Estuary During Neap Tides. Journal Coastal Research, SI 50 (Proceedings 9th International Symposium), 832 – 836. Gold Coast, Australia, ISSN 0749.0208 Significant changes sediment concentration shear stress can occur within an estuarine turbidity maximum. Prediction mud transport depends on a good specification settling...

10.2112/jcr-si50-155.1 article EN Journal of Coastal Research 2007-06-30

Abstract High quality laboratory measurements of nearshore waves and morphology change at, or near prototype-scale are essential to support new understanding coastal processes enable the development validation predictive models. The DynaRev experiment was completed at GWK large wave flume over 8 weeks during 2017 investigate response a sandy beach water level rise varying conditions with without dynamic cobble berm revetment, as well resilience revetment itself. A array instrumentation used...

10.1038/s41597-021-00805-1 article EN cc-by Scientific Data 2021-01-20

It is projected that global mean sea level could rise up to 1 m this century with a strong regional pattern. estimated 20percent of England’s coastal defenses fail under just half rise. Ambitious climate mitigation and adaptation plans may protect 400,000 – 500,000 people, but flood erosion risks cannot be fully eliminated. Building resilience requires accurate wave overtopping prediction tools nowcast information prepare for respond hazards. In Dawlish, SW England, new monitoring system...

10.9753/icce.v37.papers.1 article EN Coastal Engineering Proceedings 2023-09-01

Cet article présente une campagne expérimentale internationale de grande envergure qui s'est déroulée en Mars-Avril 2008 sur la côte aquitaine.Cette a permis mettre oeuvre des instrumentations et méthodes innovantes afin mesurer vaste gamme processus hydrodynamiques, sédimentaires morphologiques zone surf jet rive tout couvrant échelles temporelles milli secondes à plusieurs semaines spatiales subcentimétriques décamétriques.Cette apportera un jeu données unique avec conditions énergétiques...

10.5150/jngcgc.2008.061-s article FR 2008-01-01
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