What influences the weather in Britain?
Britain has a temperate maritime climate. It is a maritime climate as the sea influences the type of weather we receive. This means that on average we have warm, wet summers and cool but fairly mild winters.
Our close proximity to the Atlantic Ocean, the presence of the Gulf Stream (a warm current in the Atlantic) and our northern latitude are the three principle factors influencing the weather of the British Isles. The Gulf Stream is the reason why the British Isles are a lot warmer than other countries at the same latitude including Canada and Russia.
The prevailing (dominant) winds flow from the south-west bring moist warm air transported via the Gulf Stream. As a result the western side of the country is the wettest, particularly areas of high relief such as Wales, Scotland and the Lake District which experience orographic rainfall.
Temperatures are largely controlled by latitude, varying from an average of 10.8 °C in the south and a cooler 7.9 °C in Aberdeen in the north of Scotland. In the summer the latitudinal temperature difference can be as much as 5 °C and they are marginally lower on the west coast due to the cooling effect of the prevailing winds. By contrast, in the summer the west coast is generally warmer as the water warms the prevailing winds.
The Gulf Stream
BBC TV Series
The BBC’s The Great British Weather live show aired earlier this summer provides inspiration for creating fascinating weather and climate lessons. The link below, entitled ‘The Battle of the Weather Fronts’ is a short film clip of rugby player’s acting out as the 4 major air masses that influence Britons weather. This has an element of fun about it and I expect it will appeal to boys in particular. To benefit all of the kinaesthetic learners, this battle of the air masses could be played out on the school field (also a good way to wake up any sleepy heads on a Monday morning).
The Big Freeze of 2010
Satellite image of the British Isles under a blanket snow, captured on the 7th of January 2010 from the NASA Earth Observatory. |
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