How does continentality affect climate in a given region

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Conrad, V. Usual formulas for continentality and their limits of validity. American Geophysical Union Transactions , 27 : — Google Scholar. Continentality in the Western United States. Bulletin of the American Meteorological Society , 36 : — Driscoll, D. Yee, Continentality: a basic climatic parameter re-examined. International Journal of Climatology , 12 — Fobes, C. Winds that blow to Britain from warm inland areas such as Africa will be warm and dry.

Winds that blow to Britain from inland areas such as central Europe will be cold and dry in winter. Britain's prevailing i. These winds are cool in the summer, mild in the winter and tend to bring wet weather. Climate can be affected by mountains.

Mountains receive more rainfall than low lying areas because as air is forced over the higher ground it cools, causing moist air to condense and fall out as rainfall. The higher the place is above sea level the colder it will be. This happens because as altitude increases, air becomes thinner and is less able to absorb and retain heat. That is why you may see snow on the top of mountains all year round. The distance from the equator affects the climate of a place. At the poles, energy from the sun reaches the Earth's surface at lower angles and passes through a thicker layer of atmosphere than at the equator.

This means the climate is cooler further from the Equator. The poles also experience the greatest difference between summer and winter day lengths: in the summer there is a period when the sun does not set at the poles; conversely the poles also experience a period of total darkness during winter.

In contrast, daylength varies little at the equator. The warmer water pumps energy and moisture into the atmosphere, altering global wind and rainfall patterns. The phenomenon has caused tornadoes in Florida, smog in Indonesia, and forest fires in Brazil. The factors above affect the climate naturally. However, we cannot forget the influence of humans on our climate. Central areas of continents are dry because air moving over landmasses does not absorb large amounts of water vapour.

Weather is day-to-day information of the changes in the atmospheric condition in any area. Climate is statistical weather information that provides information about the average weather condition of a particular place over a long period. The changes in the weather condition can be observed very frequently.

Continentality — in winter, the sea insulates the islands as it cools more slowly than the land and this helps to keep the UK warmer than most other countries of the same latitude. Coastal areas are warmer than inland areas in winter, because the sea retains heat and warms up the land.

The continental effect is a phenomenon that causes temperatures in inland areas to fluctuate more than temperatures near to large bodies of water.