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Climate Change and the European Water Dimension - Agri ...

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Mountain lakes can be found in most of Mediterranean countries like Italy, France,<br />

Spain, Albania, <strong>and</strong> Greece where <strong>the</strong>y should be allocated to alpine ra<strong>the</strong>r than to<br />

Mediterranean types.<br />

The most important Italian lake district is located in nor<strong>the</strong>rn Italy <strong>and</strong> includes <strong>the</strong><br />

deep sub alpine lakes <strong>and</strong> some small-medium Insubrian lakes, which toge<strong>the</strong>r make<br />

up more than 80% of <strong>the</strong> total volume of lakes in Italy (Premazzi et al., 2003). One of<br />

<strong>the</strong> most important hydrodynamic features in <strong>the</strong> great lakes (i.e. Como, Garda,<br />

Maggiore) is <strong>the</strong>ir specific holo-oligomixis. The rainfall regime in this area is typical of<br />

<strong>the</strong> Alpine Region with <strong>the</strong> precipitation maximum between May <strong>and</strong> November.<br />

Approximately 70-75% of <strong>the</strong> annual precipitation volume is concentrated to this<br />

period. The climate is of continental type.<br />

The Central Italian lakes belong to <strong>the</strong> Middle Thyrrenian Climatic District, <strong>and</strong><br />

occupy <strong>the</strong> highest part of <strong>the</strong> volcanic area characterised by a maritime climate with<br />

generally mild winters <strong>and</strong> hot summers (Ambrosetti <strong>and</strong> Barbanti, 2002). The lakes<br />

in this region are of different origin: volcanic crater lakes (like Lake Bolsena), alluvial<br />

lakes (like Lake Trasimeno) or coastal (like Lake Lesina <strong>and</strong> Lake Varano in Puglia).<br />

The Latium lakes (Bolsena, Bracciano, Nemi, Vico) have some hydrodynamic<br />

features characteristic of lakes in an oceanic climate. As a consequence of this, <strong>the</strong><br />

<strong>the</strong>rmocline in <strong>the</strong>se lakes develops much deeper than in <strong>the</strong> nor<strong>the</strong>rn district, though<br />

not as deep as in lakes with a really oceanic climate (Pompilio et al., 1996).<br />

Greek lakes can be divided into three categories: warm monomictic deep lakes,<br />

warm monomictic shallow lakes, <strong>and</strong> dimictic shallow lakes (Zacharias, 2002).<br />

Spanish lakes range by <strong>the</strong>ir salinity level from freshwater to hypersaline lakes <strong>and</strong><br />

by <strong>the</strong>ir permanency from ephemeral, filled with water for less than one month, to<br />

deep stratified permanent lakes. Temporary lakes with increased salt content are<br />

characteristic of endorheic basins (without outflow) in semi-arid <strong>and</strong> arid climate<br />

zones while permanent lakes are located at higher altitudes <strong>and</strong> in carstic areas.<br />

Besides natural lakes, <strong>the</strong>re are about 4000 large dams in <strong>the</strong> Mediterranean region<br />

(Table IV.B.2). The top five countries in terms of <strong>the</strong> number of dams are Spain, with<br />

1,196 large dams, or just under one third of <strong>the</strong> Mediterranean total, Turkey (625),<br />

France (569), <strong>and</strong> Italy (524) (Haas, 2002).<br />

56

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