Sources of the Levantine Intermediate Water in winter 2019
| Type | Article | ||||||||
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| Date | 2022-06 | ||||||||
| Language | English | ||||||||
| Author(s) | Taillandier V. 1, D’ortenzio F.1, Prieur L1, Conan P.2, Coppola L.1, Cornec M.1, Dumas F3, Durrieu De Madron X.4, Fach B.5, Fourrier M.1, Gentil M.4, Hayes D.6, Husrevoglu S.5, Legoff H.7, Le Ster L.1, 8, Örek H.5, Ozer T.9, Poulain P.M.10, Pujo‐pay M.2, Ribera D’alcalà M.11, Salihoglu B.5, Testor P.7, Velaoras D.12, Wagener T.13, Wimart‐rousseau C.13 |
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| Affiliation(s) | 1 : Sorbonne Université CNRS Laboratoire d’Océanographie de Villefranche (LOV) 06230 Villefranche‐sur‐Mer ,France 2 : Sorbonne Université CNRS Laboratoire d’Océanographie Microbienne (LOMIC) 66650 Banyuls‐sur‐Mer ,France 3 : Service Hydrographique et Océanographique de la Marine (SHOM) 29200 Brest ,France 4 : CEFREM CNRS Université de Perpignan Via Domitia 66860 Perpignan, France 5 : Middle East Technical University (METU) Institute of Marine Sciences 33731 Erdemli‐Mersin ,Turkey 6 : Oceanography Center University of Cyprus 1678 Nicosia, Cyprus 7 : Sorbonne Université CNRS IRD MNHN Laboratoire d’Océanographie et de Climatologie (LOCEAN) 75005 Paris ,France 8 : Centre d’Etudes Biologiques de Chizé (CEBC) CNRS ,France 9 : Israel Oceanographic & Limnological Research (IOLR) 31080 Haifa, Israel 10 : National Institute of Oceanography and Applied Geophysics (OGS) 34010 Sgonico (TS) ,Italy 11 : Stazione Zoologica Anton Dohrn (SZN) Villa Comunale80121 Napoli, Italy 12 : Hellenic Center for Marine Research (HCMR) Institute of Oceanography 19013 Anavyssos,Greece 13 : Aix Marseille Université Université de Toulon CNRS IRD MIO Marseille, France |
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| Source | Journal Of Geophysical Research-oceans (2169-9275) (American Geophysical Union (AGU)), 2022-06 , Vol. 127 , N. 6 , P. e2021JC017506 (19p.) | ||||||||
| DOI | 10.1029/2021JC017506 | ||||||||
| WOS© Times Cited | 4 | ||||||||
| Keyword(s) | descriptive oceanography, overturning circulation, Mediterranean Sea, ocean observations, water mass formation, Levantine intermediate water | ||||||||
| Abstract | Climatic changes and interannual variability in the Mediterranean overturning circulation are crucially linked to dense water formation in the Levantine Sea, namely the Levantine Intermediate Water whose formation zone, comprising multiple and intermittent sources, extends over fluctuating pathways. To probe into the variability of this water formation and spreading, a unique dataset was collected during the winter of 2019 in the western Levantine Sea, via oceanographic cruises, profiling floats and a glider, at a spatio-temporal distribution suited to resolve mesoscale circulation features and intermittent convection events. This study highlights the competition between two source regions, the Cretan Sea and the Rhodes Cyclonic Gyre, to supply the Mediterranean overturning circulation in Levantine Intermediate Water. The Cretan source was estimated as the most abundant, supported by increasingly saltier water masses coming from the Levantine Sea under the pumping effect of a water deficit caused by strong western outflow towards the Ionian Sea. Key Points Descriptive oceanography of the Levantine Intermediate Water formation zone using an in-situ multiplatform approach Competition between two source regions to supply the Mediterranean overturning circulation in Levantine Intermediate Water The Cretan Sea is the most abundant source, supported by increasingly saltier waters coming from the Levantine Sea Plain Language Summary The Mediterranean overturning circulation is a conveyor belt transporting salt from its easternmost areas towards the North Atlantic Ocean. To explore how the formation of dense and salty waters called the Levantine Intermediate Water fits into this circulation, the western Levantine Sea was investigated during the winter of 2019 via cruise surveys and an array of autonomous sensors. This study highlights the competition between two source regions, the southern Aegean Sea and the northwestern Levantine Sea, to supply the Mediterranean overturning circulation in Levantine Intermediate Water. In the period under study, the first region was estimated as the most abundant source. This source was supported by increasingly saltier water masses coming from the Levantine Sea, under the pumping effect of a water draught in the Aegean Sea. These observations help to nuance the complex picture of Levantine circulation patterns which are subject to large variability. |
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