Friday, 24 September 2010
The Final Hours
Friday, 17 September 2010
Evidence for Global Warming..
- Instrument readings - measurements made using at weather stations suggest a clear increasing trend. Figures show that temperatures have increased globally by 0.5 degrees since 1980.
- Arctic Ice Cover - studies have shown that over the last 30 years, Arctic Ice has thinned to nearly half its previous level. As the ice retreats less solar radiation is reflected back into space. Darker ocean areas will absorb more radiation, increasing temperatures further.
- Glacier retreat - photographic evidence has shown clear glacial retreat over the last century. Studies have estimated that up to 25% of global mountain glaciers could disappear by 2050. However, a natural reduction in snowfall could also lead to glacial retreat.
- Ice Cores - Ice cores have provided some of the most compelling evidence for global warming. Similar to tree rings in their formation they display a a visual record of snow fall. Gas molecules trapped in the ice can also be analysed to discover the atmospheric conditions at the time of formation.
Extreme Weather in the UK
- 2003 - Europe suffered an intense heatwave. The highest temperature recorded in the UK was 38.5 degrees Celsius.
- 2007 - Floods across the UK, in particular Hull and Sheffield, caused many thousands of people damage and loss of homes. Not only did rivers burst their banks but pumping stations also failed due to the sheer volume of water.
- 2008 - Further floods occurred as torrential rain fell on already saturated ground. The most affected areas were Somerset and Northumberland.
Friday, 10 September 2010
Numeracy
Thursday, 9 September 2010
Apologies
Wednesday, 28 July 2010
UK Weather
What causes the weather in the UK?
The two major atmospheric characteristics that are the reason for the majority of the weather in the UK are depressions and anticyclones.
A depression is an area of low pressure. Air rises leading to the formation of clouds and rain. UK weather is associated with the movement of depressions across the land. Depressions form over the Atlantic Ocean and pass from West to East across the UK driven by the prevailing winds. Depressions form at the boundary between cold polar air moving South and warm tropical air moving North and is known as the polar front. Once formed, the air begins to rotate, spiralling upwards in an anti-clockwise direction forming clouds and then rain.
Within a depression there are two further ‘fronts’, one cold and one warm. The warm front signifies the front of the warmer air (hence the name, genius!) and the cold front........you get the idea. As the depression builds it eventually dies out as the cold front catches up with the slower warm front. As depressions pass over the UK a sequence of weather is produced. At the front of the depression a steady rain falls. Behind this, small patches of rain begin to fall as the temperature rises slowly due to the warm air. The advancing cold front causes the temperature to drop and the rain ceases.
Unlike depressions, anticyclones are areas of high pressure cause by descending air. The chances of rain are slim as the descending air prevents air from rising and therefore forming clouds. Winds also travel clockwise, the opposite of depressions. Anticyclones can be separated further into two main types, winter and summer anticyclones. In winter, cloudless skies result in bright but cold conditions. As there is no cloud heat it lost rapidly into the atmosphere and this is what causes frost to appear on the ground in the early morning. If the air is particularly heavy with moisture from the surrounding seas then can condense into mist and fog. In the summer time the sun is much stronger due to Earths’ rotation on its axis and is easily able to burn away and resulting mist and fog. Summer anticyclones typically result in dry, sunny conditions (of which we see very little these days). The below diagram is a basic example of an anticyclone situated over the UK.
Tuesday, 20 July 2010
Rain, Rain, Go Away!
In the next ‘block’ of posts I’m going to discuss aspects of weather and climate, in particular focusing on the UK. The UK may be the obvious choice, however, it is important that students can relate to a particular topic as such they will all have experience of the British weather. I was swayed to discuss climate next as I have just returned from work and unfortunately endured a soaking on the way.
The climate of the UK is largely influenced by its physical position. The UK lies at the forefront of confrontation between descending polar air from the North and rising sub-tropical weather from the South. As a result we experience varied weather conditions throughout the year. The below image shows the major air flows which circulate Earth.
There are a number of other factors that the climate of the UK. These include:
- The North Atlantic Drift - a warm ocean current that provides the UK with relatively warm winters considering our latitude.
- Prevailing winds - typically flowing in from the south-west, these, along with the North Atlantic Drift result in a warm but wet climate.
- The relief of the UK - as air is forced upwards in upland areas the temperature decreases and clouds form causing subsequent rainfall and hence why the Lake District and the majority of Scotland typically have a large number of rainy days a year. The below diagram is a excellent illustration of how relief rainfall works.
As I have mentioned in my previous posts I believe that before beginning to teach a new topic it is important to have a knowledge of what the students already know. For climate in the UK a possible idea would be to provide a trace of the coastline and then suggest students to shade areas of the UK which they believe to be typically wet in blue, and the warm areas in red. Discussion on why they had chosen those areas would allow the teacher to get a good insight into current understanding.
As a final point I found the Met Office website to be an extremely valuable resource when researching this topic. It contains a huge amount of data available in an instant and even provides basic lesson plans, including presentations and slide shows, which introduce certain topics.