PHYSICOCHEMICAL INTERACTIONS BETWEEN THE ADRIATIC AND THE IONIAN SEAS Ekaterini Souvermezoglou 1* and Evangelia Krasakopoulou 1 1 Hellenic Centre for Marine Research Institute of Oceanography -
[email protected] Abstract The ability of the Adriatic in renewing the deep waters of the Eastern Mediterranean is investigated in relation to the properties of the LIW entering from the Ionian Sea. This study is based on oxygen and nutrient data collected in the Otranto strait and the surrounding area between 1987 and 2000. Keywords: Oxygen, Nutrients, Intermediate waters, Otranto Strait The Adriatic Sea is a semi-enclosed basin shallow in the north and deep in the south. It communicates with the Ionian Sea thought the Strait of Otranto, a 70 km wide and 800 m deep channel. The general circulation in the Adriatic basin is cyclonic [1] consisting from a rather weak current along the eastern coast (the Eastern Adriatic Current - EAC) and a fast mainly coastal current along the western coast (the West Adriatic current - WAC). The Ionian Sea is a deep (up to 4000m) and wide basin which receives salty and warm waters from the easternmost part of the Mediterranean and fresher and relatively colder water from the western Mediterranean. The EAC bring Levantine Intermediate Water (LIW) and Ionian Surface Water (ISW) into the Adriatic [2]. Adriatic is prone to strong winter outbreaks of cold dry northerly winds which induce extended heat losses and evaporation, that drive to deep water formation events. During cold winters and restricted fresh water input, the densest water in the whole of the Mediterranean, the North Adriatic Dense Water (NAdDW) is formed over the shallow northern shelf of the Adriatic [3].