This study used data collected during six hydrographic cruises in the western half of the Cap Bon – Mazara del Vallo section during 2003. The analyses of transects reveals the presence of Western Intermediate Water (WIW) in April and Ionian Water (IW) in March-April on the Tunisian side of the channel in a transitional layer between Atlantic Water (AW) and Levantine Intermediate Water (LIW). The conclusions on seasonal and mesoscale variability are confirmed by a high resolution numerical simulation
11 pages, 8 figures, 1 tableThe Levantine Intermediate Water (LIW) traditionally has been assumed to...
International audienceThe mean seasonal hydrography and circulation of the Western Iberian Margin (W...
International audienceA simulation of the Mediterranean circulation between 2011 and 2020 at a resol...
International audienceStudies of water masses present in the Channel of Sicily are relevant to under...
International audienceWe analysed in situ CTD data collected on 36 joint Tunisian–Italian oceanograp...
AbstractWe analysed in situ CTD data collected on 36 joint Tunisian–Italian oceanographic cruises in...
Hydrographic changes in the western Mediterranean Sea (WMED), which is connected to the North Atlant...
Seasonality of hydrographical properties at depth in the western Iberian margin (eastern North Atlan...
8 pages, 6 figuresThe Western Intermediate Water (WIW) is probably the less studied water mass in th...
[1] Data from a hydrographic survey of the Tunisia-Sardinia-Sicily region are assimilated into a pri...
Historical oceanographic surveys carried out around the Balearic Islands (western Mediterranean) sug...
The Levantine Intermediate Water (LIW) is a main contributor to the circulation system of the Medite...
A high resolution eddy-resolving primitive equation numerical model (ROMS), is used to study the var...
Special issue PRIMO-0.-- 30 pages, 18 figuresIn the western Mediterranean Sea, the Northern Current ...
Eastern North Atlantic Central Water (ENACW, 50-400 m) and Mediterranean Over ow Water (MOW, 300 m t...
11 pages, 8 figures, 1 tableThe Levantine Intermediate Water (LIW) traditionally has been assumed to...
International audienceThe mean seasonal hydrography and circulation of the Western Iberian Margin (W...
International audienceA simulation of the Mediterranean circulation between 2011 and 2020 at a resol...
International audienceStudies of water masses present in the Channel of Sicily are relevant to under...
International audienceWe analysed in situ CTD data collected on 36 joint Tunisian–Italian oceanograp...
AbstractWe analysed in situ CTD data collected on 36 joint Tunisian–Italian oceanographic cruises in...
Hydrographic changes in the western Mediterranean Sea (WMED), which is connected to the North Atlant...
Seasonality of hydrographical properties at depth in the western Iberian margin (eastern North Atlan...
8 pages, 6 figuresThe Western Intermediate Water (WIW) is probably the less studied water mass in th...
[1] Data from a hydrographic survey of the Tunisia-Sardinia-Sicily region are assimilated into a pri...
Historical oceanographic surveys carried out around the Balearic Islands (western Mediterranean) sug...
The Levantine Intermediate Water (LIW) is a main contributor to the circulation system of the Medite...
A high resolution eddy-resolving primitive equation numerical model (ROMS), is used to study the var...
Special issue PRIMO-0.-- 30 pages, 18 figuresIn the western Mediterranean Sea, the Northern Current ...
Eastern North Atlantic Central Water (ENACW, 50-400 m) and Mediterranean Over ow Water (MOW, 300 m t...
11 pages, 8 figures, 1 tableThe Levantine Intermediate Water (LIW) traditionally has been assumed to...
International audienceThe mean seasonal hydrography and circulation of the Western Iberian Margin (W...
International audienceA simulation of the Mediterranean circulation between 2011 and 2020 at a resol...