Tidal currents in the Malta – Sicily Channel from high-frequency radar observations. (15th October 2015)

• Record Type: Journal Article
• Authors: Cosoli, Simone; Drago, Aldo; Ciraolo, Giuseppe; Capodici, Fulvio
• Is Part Of: Continental shelf research. Volume 109(2015)
• Page Start: 10
• Page End: 23
• Publication Date: 2015-10-15
• Subjects: HF coastal radars -- Sicily Channel -- Tides -- Tidal currents -- Mediterranean Sea; Continental shelf -- Periodicals; Submarine geology -- Periodicals; 551.41
• DOI: 10.1016/j.csr.2015.08.030
• Languages: English
• ISSNs: 0278-4343

Abstract

Abstract: Two years of sea surface current measurements acquired since August 2012 by High-Frequency SeaSonde radars over the relatively shallow shelf area dividing the Maltese Islands from Sicily (the Malta - Sicily Channel), are used to characterize the surface tidal currents in the region. Tidal currents are generally weak and concentrated in the semidiurnal and diurnal bands, barely exceeding 3 cm s −1 in the semidiurnal band (M2, S2 ), and below 6 cm s −1 in the diurnal band (K1, O1 ). In the middle part of the basin, the M2 currents oscillate along the main Channel axis; on the contrary the S2 oscillations are oriented along the energetic Atlantic Ionian Stream (AIS) flow. Diurnal tides have a more circular pattern, also following the AIS path and with a significant intensification in proximity of the shelf break, thus suggesting a substantial contribution from internal tides in the region. Phase contours suggest the presence of amphidromic points for both the semidiurnal and diurnal constituents, located in the central area of the Channel for S2, O1 and K1, but slightly shifted towards north-west for the M2 component. Highlights: A novel data set of sea-surface currents in the Sicily Channel is introduced and an interpolation technique is described. Tidal currents in the central mediterranean sea are investigated. Tidal currents are weak and concentrated in the diurnal–semidiurnal band. Diurnal-period tidal currents are potentially affected by internal tides.