Regional Climates of the British Isles
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North Atlantic Drift (Gulf Stream)
Regional Climates of the British Isles. Julian Mayes ; Dennis Wheeler. Publisher: Routledge , This specific ISBN edition is currently not available. View all copies of this ISBN edition:. Synopsis About this title Global climate and the effects of global warming are commanding unprecendented interest as climates grow more dynamic and changeable.
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Weather and climate
Without this steady stream of warmth the British Isles winters are estimated to be more than 5C cooler, bringing the average December temperature in London to about 2C. At the end of the last Ice Age, when the ice sheet covering North America melted, the sudden increase in fresh water reduced the salinity of the north Atlantic surface water and therefore less 'dense water' sank and moved towards the equator.
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This reduced, or even shut-down completely, the warm Gulf Stream. Temperatures in north-west Europe fell by 5C in just a few decades.
This is one source of cold dense water that drives the density-based component of the Gulf Stream. There may be an increase in flow from other cold water sources, but, if not, it could be the start of the slow down of the Gulf Stream. This slowing will have a cooling effect but the temperature will still increase in the region overall.
British Weather and Climate
It suggests that the British Isles, especially western regions, will see a significantly smaller temperature increase than other areas of land mass. Climatic distinctiveness and local weather contrasts are described for each region, together with a summary of climatic data from to the present. Reviewing the history and causes of climatic change and evaluating regional models, Regional Climates of the British Isles offers an important analysis of climatic variations. Examining future climatic change and its likely consequences, the authors acknowledge the need for regionally diverse responses to the greenhouse effect.
excurticana.ga Regional Perspectives on Climatic Variability and Change.