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Weather and Climate Part 1 - Introduction CGF3M Crescent School Definitions • Weather: all the atmospheric activities that occur at a given place at a given time. The condition of the atmosphere. • Climate: atmospheric conditions a place has, averaged over a long period of time. The average of weather. • Include: temperature, wind speed and direction, humidity, precipitation, pressure, cloud cover. Weather: •Short Term •Small Scale •Difficult to predict and forecast (Daily) •Temperature, Precipitation, Humidity, Wind direction and speed, pressure •Meteorology Climate: •Long Term •Large Scale •Easy to predict (Seasonal) •Climate is the averages of Temperature, Precipitation etc. •Climatology 07_00CO.JPG Climatic Controls It is obvious that not all places on earth experience the same weather or climate. There are a number of factors that effect the weather or climate. They are called ‘Climatic Controls’. Remember Grade 9 and LOWER - Near Water! This year we will change it up a bit. There are Four basic variables that influence climate: 1. Insolation: amount of solar radiation a place receives (amount of daylight & angle of suns rays - Latitude) 2. Elevation: Altitude (air pressure/heat released) 3. Proximity of water bodies: (moderates, continental areas with large lakes) 4. Ocean currents: movement of heat from the equator toward the poles (temperature & precipitation) Microclimates • Subtle variations in temperature, humidity and precipitation on a small scale. – Exposure: influence of wind on temperature and humidity – Albedo: surfaces convert solar energy into heat • Walk (outside) around the school one day and you will notice surprisingly different conditions around the area that contains the school • Dark Pavement • Natural cover - grass, trees etc. • Strong Sun • The Shade • Buildings acting as barriers to the sun or wind Exposure: • Slopes - southern slopes receive more sun than northern slopes • Wind Chill - how cold the temperature feels to people because of the wind. • A surface that is heated by the sun will be cooled quickly if there is a strong wind that blows the heated air away quickly. This type of surface will also dry faster. Albedo: • Dark surfaces convert more of the available heat than light surfaces. Walk across black pavement with bare feet on a hot summer day, then walk on grass. • Objects with low albedo are cooler than objects with high albedo Urban Heat Island: Concrete Tall buildings - wind tunnels Cars, air conditioners Subways Pollutions - Inversions Increased levels of Carbon Dioxide, Carbon Monoxide, Nitrous oxide etc. Many cities that have large parks and ravines compensate this Urban Heat Island effect. The End Go to Part 2 of the Weather and Climate slide shows