Geographical position of Great Britain is rather good as the country lies on the crossways of the see routes from Europe to other parts of the world. The sea connects Britain with most European countries such as Belgium, Holland, Denmark, Norway and some other countries. The main sea route from Europe to America also passes through the English Channel.
Great Britain enjoys the humid and mild marine West-Coast climate with warm winters and cool summers and a lot of rainfall throughout the year.
The prevailing winds blow from the south-west. As these winds blow from the ocean, they are mild in winter and cool in summer, and are heavily charged with moisture at all times. As they approach the mountainous areas near the west coasts, they rise up the mountain slopes. Their temperature drops, which causes condensation of moisture in the form of rain. Therefore the wettest parts of Britain are those areas where high mountains lie near the west coast: the western Highlands of Scotland, the Lake District and North Wales. The eastern part of Britain is said to be in the rain-shadow, as the winds lose most of their moisture in their passage over the highlands of the west.
As to temperature, Great Britain has warmer winters than any other district in the same latitude. It is due in large measure to the prevalence of mild southwest winds. Another factor is the Gulf Stream, which flows from the Gulf of Mexico and brings much warmth from the equatorial regions to north-western Europe.
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Geographical position of Great Britain is rather good as the country lies on the crossways of the see routes from Europe to other parts of the world. The sea connects Britain with most European countries such as Belgium, Holland, Denmark, Norway and some other countries. The main sea route from Europe to America also passes through the English Channel.
Great Britain enjoys the humid and mild marine West-Coast climate with warm winters and cool summers and a lot of rainfall throughout the year.
The prevailing winds blow from the south-west. As these winds blow from the ocean, they are mild in winter and cool in summer, and are heavily charged with moisture at all times. As they approach the mountainous areas near the west coasts, they rise up the mountain slopes. Their temperature drops, which causes condensation of moisture in the form of rain. Therefore the wettest parts of Britain are those areas where high mountains lie near the west coast: the western Highlands of Scotland, the Lake District and North Wales. The eastern part of Britain is said to be in the rain-shadow, as the winds lose most of their moisture in their passage over the highlands of the west.
As to temperature, Great Britain has warmer winters than any other district in the same latitude. It is due in large measure to the prevalence of mild southwest winds. Another factor is the Gulf Stream, which flows from the Gulf of Mexico and brings much warmth from the equatorial regions to north-western Europe.
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