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Climate and Weather CGC1P
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Weather The day to day characteristics of atmospheric conditions
Temperature Precipitation (rain, snow) Humidity Wind speed and direction Air Pressure
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Climate The long term pattern of weather conditions
Over the years, records have been kept of the weather in different part of Canada These records show a pattern over a long period of time Climate influences: Where we live What we grow Clothes we wear Outdoor activities
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Measuring the Weather Precipitation – rain gauge
Temperature – thermometer in Celsius Humidity (moisture in air) – hygrometer Wind – anemometer Cloud cover – satellites Air pressure – barometer UV rating Wind direction – weather vane
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Climate Factors Remember the acronym “LOWERN” or “Lower Near Water” to help remember the six major influences of a region’s climate Lattitude Ocean Currents Wind Elevation and Relief Nearness to Water
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Lattitude Distance from the equator is the major determining factor in whether a region is hot or cold Why? Recall: the sun’s energy is more concentrated at the equator while the same amount of sunlight must heat a much greater area in the poles (curvature of the earth) In general terms, the further the distance from the poles, the colder the temperature
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Ocean Currents The temperature of air above the water is affected by the type of current Example: cold current = cold air temperature Labrador current – cold current Gulf of Mexico – warm current North Pacific – warm current
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Wind Jet stream – flows up to 400 km/h at altitude of 8000 m to m flows west to east in the Northern Hemisphere Origin of wind can bring dry, cold air (polar) or warm, moist air (Gulf of Mexico)
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Elevation and Relief Relief refers to differences in elevation
Mountain ranges act as barriers to movement of air masses AND cause precipitation
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Elevation and Relief Air cools as it rises
Drops 1 degree for every 100 m elevation increase After condensation begins (cloud formation) the temperature drop is .60 degrees for every 100m increase
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Nearness to Water Water can have a moderating effect on land temperatures WHY? Water takes much longer to heat up AND cool than land
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Example: Vancouver Summer: Winter:
water is much cooler than land = cooler temperatures in Vancouver Winter: water temperature is warmer than land = warmer temperatures on land than would normally occur Vancouver has what we call a Maritime Climate – water moderates the temperature producing a small temperature range
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