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Theocharis A. Plomaritis

Researcher at University of Cádiz

Publications -  62
Citations -  1408

Theocharis A. Plomaritis is an academic researcher from University of Cádiz. The author has contributed to research in topics: Storm & Overwash. The author has an hindex of 16, co-authored 56 publications receiving 973 citations. Previous affiliations of Theocharis A. Plomaritis include National Oceanography Centre & National Oceanography Centre, Southampton.

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Sandy coastlines under threat of erosion

TL;DR: In this article, the authors show that ambient trends in shoreline dynamics, combined with coastal recession driven by sea level rise, could result in the near extinction of almost half of the world's sandy beaches by the end of the century.
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Beachrock occurrence, characteristics, formation mechanisms and impacts

TL;DR: In this paper, the authors present a review of the reported occurrences, characteristics and formation mechanisms of beachrocks and consider their impacts on the coastal zone, which is a global and diachronic phenomenon and the great majority of beachrock formations are found in tropical/subtropical and low temperate latitude, microtidal coasts.
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Predicting coastal hazards for sandy coasts with a Bayesian Network

TL;DR: In this article, a probabilistic Bayesian Network (BN) is proposed to predict the impact of a storm on sandy coast by using the hydraulic boundary conditions, characteristics of the coastal zone, and onshore hazards.
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Establishing storm thresholds for the spanish gulf of Cádiz coast

TL;DR: In this paper, critical thresholds for storm impacts along the Spanish coast of the Gulf of Cadiz were defined by computing theoretical sea-level variations during storms and comparing them with the topography of the study area and the location of infrastructure at a local level.
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Coastal barrier stratigraphy for Holocene high-resolution sea-level reconstruction.

TL;DR: The stratigraphy of a sandy barrier is explored to identify the best sea-level indicators and provide a new sea- level reconstruction for the central Portuguese coast over the past 6.5 ka, showing good agreement with previous studies, including the Tagus isostatic model, with minor discrepancies that demand further improvement of regional models.