Abstract. Due to the semi-enclosed nature of the Mediterranean Sea,
natural disasters and anthropogenic activities impose stronger pressures on
its coastal ecosystems than in any other sea of the world. With the aim of
responding adequately to science priorities and societal challenges,
littoral waters must be effectively monitored with high-frequency radar
(HFR) systems. This land-based remote sensing technology can provide, in
near-real time, fine-resolution maps of the surface circulation over broad
coastal areas, along with reliable directional wave and wind information.
The main goal of this work is to showcase the current status of the
Mediterranean HFR network and the future roadmap for orchestrated actions.
Ongoing collaborative efforts and recent progress of this regional alliance
are not only described but also connected with other European initiatives
and global frameworks, highlighting the advantages of this cost-effective
instrument for the multi-parameter monitoring of the sea state. Coordinated
endeavors between HFR operators from different multi-disciplinary
institutions are mandatory to reach a mature stage at both national and
regional levels, striving to do the following: (i) harmonize deployment and maintenance
practices; (ii) standardize data, metadata, and quality control procedures;
(iii) centralize data management, visualization, and access platforms; and (iv) develop practical applications of societal benefit that can be used for
strategic planning and informed decision-making in the Mediterranean marine
environment. Such fit-for-purpose applications can serve for search and
rescue operations, safe vessel navigation, tracking of marine pollutants,
the monitoring of extreme events, the investigation of transport processes,
and the connectivity between offshore waters and coastal ecosystems.
Finally, future prospects within the Mediterranean framework are discussed
along with a wealth of socioeconomic, technical, and scientific challenges
to be faced during the implementation of this integrated HFR regional
network.
The dynamics of the Sicily Channel and the southern Tyrrhenian Sea are highly influenced by the seasonal variability of the Mediterranean basin-wide circulation, by the interannual variability of the numerous mesoscale structures present in the Channel, and by the decadal variability of the adjacent Ionian Sea. In the present study, all these aspects are investigated using in-situ (Lagrangian drifter trajectories and Argo float profiles) and satellite data (Absolute Dynamic Topography, Sea Level Anomaly, Sea Surface Temperature, wind products) over the period from 1993 to 2018. The availability of long time series of data and high-resolution multi-sensor surface currents allow us to add new details on the circulation features and on their driving mechanisms and to detect new permanent eddies not yet described in literature. The structures prevailing in winter are mainly driven by wind, whereas those prevailing in summer are regulated by topographical forcing on surface currents. The strength of the surface structures located at the western entrance of the Ionian Sea and of the mesoscale activity along the northern Sicily coast is modulated by the large-scale internal variability. The vertical hydrological characteristics of these mesoscale eddies are delineated using the Argo float profiles inside these structures.
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Four sandy beaches on the island of Malta in the Central Mediterranean were regularly sampled for Large MicroPlastic (LMP) particles having a diameter between 1 mm and 5 mm, at stations located at the waterline and 10 m inshore. The 10975 extracted LMP particles were characterised (dimensions, surface roughness, colour) through unaided visual observation, microscopic analyses, and an algorithm developed within the current study. Two-thirds of the isolated particles were smooth and the majority of these belonged to the grey-white colour category, with a low degree of opaqueness and discolouration, and a high degree of transparency, suggesting that these were dominated by low-density polyethylene LMPs. Conflicting evidence concerning the relative residence time of the isolated LMPs within seawater emerged from the colour and contour roughness determination, although an abundance of primary LMPs (production pellets) within our sample might have been responsible for the low contour roughness results obtained. Roughly six times as many particles were recorded within the inshore sampling stations as the particles recorded at the waterline stations. The developed algorithm performed very well when the dimension and colour parameter values it delivered were compared with those obtained by microscopic analyses. Highlights ► No universal methodology of high validity for analysing isolated microplastics. ► Use of image processing techniques to automatically extract parameters for LMPs. ► Make the process less timeconsuming and removes subjectivity. ► Samples collected from a number of popular beaches around the island of Malta. ► Algorithm performed well in determining the dimensions and colour of the LMPs.
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