Module 1- Weather Flashcards
Temperature
Thermometer
Degrees Celsius
Rainfall
Rain Gauge
Millimetres
Wind Speed
Anemometer
Kmph / Knots
Wind Direction
Wind Vane
N / S / E / W
Cloud Cover
Observation
OCTAS
Visibility
Observation
Metres / kilometres
Sunshine
Sunshine Recorder
Hours
Air Pressure
This describes the weight of the air
High Pressure
This is Heavy sinking air. It brings clear, sunny, calm, settled weather, HOT IN SUMMER, but COLD AND FROSTY IN WINTER. Areas of High Pressure are called ANTI-CYCLONES
Low Pressure
This is lighter rising air. It brings cloudy, windy and unsettled weather, COOL IN SUMMMER but MILD IN WINTER.
Areas of low pressure are called DEPRESSIONS
Urban areas (Cities) such as Glasgow may be warmer than the surrounding countryside due to
Heating from buildings
- Heat from car engines.
- Buildings provide shelter from the wind.
Rural areas in the countryside may be slightly cooler for the following reasons:
No heat from buildings or cars.
- Trees and vegetation soak up moisture and cool the area down.
- Lakes and rivers also cool the area.
Climate
This describes the average weather which an area experiences over a period of around 30 yeas.
In the North West Highlands of Scotland, the climate is cool and wet for the following reasons:
Latitude: It is cool because it is further North from the equator.
Prevailing Winds: It is near the Atlantic Ocean and the frequent Westerly winds blow in moist air bringing cloud and rain.
Relief: The tall mountains have cooler temperatures and more rainfall.
In contrast the South East of England has much warmer drier weather for the following reasons:
Latitude: It is warmer as it is over 500miles further South, nearer the equator.
It is further from the Atlantic Ocean so is not affected by the wet westerly winds.
It has flat land with warmer temperatures and less rainfall than the mountains.