Total estimated volume of water contained in glacier ice in a given river basin. A glacier is defined as the "mass of land ice flowing down a slope (by deformation of its internal structure and by sliding at its base) and enclosed by topographic elements (such as the slopes of a valley or adjacent peaks) surrounding it. The topography of the bedrock is the most influential factor in the dynamics of a glacier and in the slope of its surface. A glacier subsists because of the massive accumulation of snow, which is compensated by the melting of ice at low altitudes or discharge into the sea".
Subdepartment of Environment Statistics - National Statistics Institute
Directorate-General of Water (DGA)
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Hydrometric Network
Annual
Administrative record
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Subdepartment of Environment Statistics - National Statistics Institute
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Annual
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Cubic kilometers (km3)
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Total estimated volume of water contained in glacier ice in a given river basin. A glacier is defined as the "mass of land ice flowing down a slope (by deformation of its internal structure and by sliding at its base) and enclosed by topographic elements (such as the slopes of a valley or adjacent peaks) surrounding it. The topography of the bedrock is the most influential factor in the dynamics of a glacier and in the slope of its surface. A glacier subsists because of the massive accumulation of snow, which is compensated by the melting of ice at low altitudes or discharge into the sea".
Subdepartment of Environment Statistics - National Statistics Institute
Administrative record
Directorate-General of Water (DGA)
Hydrometric Network
Annual
-
Cubic kilometers (km3)
-
-
-
Annual
-
-
-
-
Subdepartment of Environment Statistics - National Statistics Institute
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