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

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Chapter III. The Hydrologic Cycle<br />

III.1. INTRODUCTION<br />

<strong>Water</strong> covers 70% of <strong>the</strong> Earth’s surface, <strong>and</strong> is present in <strong>the</strong> atmosphere <strong>and</strong> <strong>the</strong><br />

crust; it also comprises a large part of all living matter. <strong>Water</strong> is <strong>the</strong> only natural<br />

resource that exists naturally in three forms: liquid, solid (snow, ice) <strong>and</strong> gas (clouds).<br />

Unlike most mineral resources, it is renewable it exists in an endless cycle, moving<br />

between its gaseous, liquid <strong>and</strong> solid forms. This “hydrologic cycle” comprises<br />

nature’s method of replenishing, redistributing <strong>and</strong> purifying <strong>the</strong> world's natural water<br />

resources.<br />

By hydrologic cycle we mean <strong>the</strong> circulation (<strong>and</strong> transformation) of water between<br />

<strong>the</strong> earth <strong>and</strong> <strong>the</strong> atmosphere through different pathways (Figure III.1). Being a<br />

cycle, it has no specific beginning or ending. Ra<strong>the</strong>r, liquid water from <strong>the</strong> Earth’s<br />

surface, particularly <strong>the</strong> oceans, is ei<strong>the</strong>r evaporated into a gaseous form <strong>and</strong> enters<br />

Figure III.1. The hydrologic cycle, with annual volumes of flow given in its units<br />

relative to <strong>the</strong> annual precipitation on <strong>the</strong> l<strong>and</strong> surface. Because of its negligible<br />

magnitude compared to o<strong>the</strong>r components, aerosol has been removed from <strong>the</strong> cycle<br />

(Maidment, 1993; with permission).<br />

<strong>the</strong> atmosphere as water vapor (clouds) or is dispersed in <strong>the</strong> atmosphere through<br />

aerosols. The atmospheric moisture is eventually returned to <strong>the</strong> Earth’s surface in<br />

<strong>the</strong> form of rain, snow or hail. Approximately 100,000 km 3 (about 20% of <strong>the</strong> total<br />

global annual precipitation) falls onto <strong>the</strong> l<strong>and</strong> surface of <strong>the</strong> continents. Except for<br />

that portion evaporated or transpired directly back into <strong>the</strong> atmosphere, <strong>and</strong> <strong>the</strong><br />

portion moved directly into <strong>the</strong> atmosphere through aerosols, most of <strong>the</strong> water<br />

reaching <strong>the</strong> l<strong>and</strong> surface in <strong>the</strong> form of rain, snow or hail will eventually find its way<br />

35

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