Due to the water body’s thermal capacity, tis warming process takes longer, tan that of the surrounding lands, tus providing a cooling effect during summer time. Mreover, te presence of winds, wich bring air from the ocean body; sreading out over the Isles is noticeable. Te result is definitely the presence of rain, tough there is either a warming or a cooling effect present. Dfferent regions of the greater British Isles do experience a contrast in terms of prevailing temperature and weather conditions. Tis is showcased by the despite the prevailing weather conditions i.
wnter or summer it is colder in the north, a compared to the south of the Isles. I addition to this is the fact that the western region is generally warmer than the west. Tis includes the coastline of Western Scotland and England, a well as Wales and Ireland (Rayner, 1981:18). Te latitude of the region further influences existing climatic conditions, wth the southern areas receiving more isolation than the northern areas. Tis is in terms of the sun’s angle, i relation to tilt on its axis.
Atitude matters, i terms of sea-level placement of land. Te British Isles, Wles is placed on higher ground, wth colder temperatures being experienced. Tere is influence by the average temperature fall of 0.65o Celsius for every 100 meters of altitude gained. Lsser insolation – incoming solar radiation absorbed by earth – provides a fall in temperature in relation to the prevailing air pressure levels. A increase in altitude results in a fall in air pressure, tereby affecting the rate of kinetic energy produced due limited of air molecules colliding.
Ar masses and prevailing winds, i terms of impacts, aso affect the Isles. I the prevailing winds is emanating from the north, tis leads to colder temperatures vis-à-vis winds from the south influencing an increase in temperature. I the region, te dominant prevailing wind, rferred to as the ‘westerlies’, d emanate from the Atlantic Ocean. Tey do increase the rate of evaporation through the journey, hnce gathering huge quantities of water vapor. Wrm air rises, i relation to the rise of altitude, rsulting a fall air pressure.
Tis catalyzes the formation of cloud cover, wth rain drenching the Western region of the Isles (Parker, 1992:34). Te Breccan Beacons (Wales), te rising. ..
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