Pyrenees - Climate

Climate

The amount of the precipitation the range receives, including rain and snow, is much greater in the western than in the eastern Pyrenees, because of the moist air that blows in from the Atlantic Ocean over the Bay of Biscay. After dropping its moisture over the western and central Pyrenees, the air is usually dry over the eastern Pyrenees. The winter average temperature is -2 °C (28.4 °F).

Sections of the mountain range vary in more than one respect. Some glaciers are found in the western and especially the snowy central Pyrenees, but the eastern Pyrenees are without any glaciers - with the quantity of snow falling there being insufficient to cause their development. The glaciers are confined to the northern slopes of the central Pyrenees, and do not descend, like those of the Alps, far down into the valleys, but have their greatest lengths along the direction of the mountain chain. They form, in fact, in a narrow zone near the crest of the highest mountains. Here, as in the other great mountain ranges of central Europe, there is great evidence of a much wider extension of the glaciers during the Ice Ages. The case of the glacier in the valley of Argeles Gazost, between Lourdes and Gavarnie, in the département of Hautes-Pyrénées is the best-known instance.

The snow-line varies in different parts of the Pyrenees from about 2,700 to 2,800 metres above sea level.

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