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Weather & Climate Mr. Skirbst Life Science Topic 20
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Weather
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The condition of the atmosphere in terms of heat, pressure, wind, and moisture
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Atmosphere - Mixture of gases surrounding the Earth
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Atmosphere - Mixture of gases surrounding the Earth - Four (4) distinct layers in the atmosphere
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4 Layers of Atmosphere Troposphere – (0 to 16 km) - lowest layer where most weather takes place - av. Temp. decreases - Tropopause is top boundary
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4 Layers of Atmosphere Stratosphere – (16 – 48 km) - Ozone layer absorbs UV light - Av. Temp. increases - Stratopause is top boundary
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4 Layers of Atmosphere Mesosphere – (48 – 80 km) - Protects us from meteoroids - Av. Temp. decreases (-100 o C) - Mesopause is top boundary
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4 Layers of Atmosphere Thermosphere– (80 - 3200 km) - Av. Temp. increases (> 2000 o C ) - Lower layer – Ionosphere - bounces radio signals - Upper layer – Exosphere - satellites orbit here
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Heat Energy -The sun is the sources of most of the heat in the atmosphere
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Heat Energy -The sun is the sources of most of the heat in the atmosphere - Heat is spread in 3 ways:
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Heat Energy -The sun is the sources of most of the heat in the atmosphere - Heat is spread in 3 ways: 1. Radiation – transfer by waves
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Heat Energy -The sun is the sources of most of the heat in the atmosphere - Heat is spread in 3 ways: 1. Radiation – transfer by waves 2. Conduction – by contact
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Heat Energy -The sun is the sources of most of the heat in the atmosphere - Heat is spread in 3 ways: 1. Radiation – transfer by waves 2. Conduction – by contact 3. Convection – by fluid (air too)
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Heat Energy
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Greenhouse Effect:
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Air Pressure -Force of atmosphere pushing on the Earth’s surface -Depends on air’s density
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Air Pressure -Force of atmosphere pushing on the Earth’s surface -Depends on air’s density -3 factors affecting air pressure
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Air Pressure 1.Temperature - as temp increases, air pressure decreases
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Air Pressure 2.Water Vapor - moisture in air - as water vapor increases, air pressure decreases
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Air Pressure 3.Altitude - elevation above sea level - as altitude increases, air pressure decreases
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Wind - Movement of air due to differences in air pressure resulting from unequal heating of the atmosphere
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Wind 2 Types of wind: 1.Local Wind (short distances)
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Wind 2 Types of wind: 1.Local Wind (short distances) Sea breeze – from sea to land
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Wind 2 Types of wind: 1.Local Wind (short distances) Sea breeze – from sea to land Land breeze – from land to sea
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Wind 2 Types of wind: 2.Global Wind (long distances) Coriolis Effect – shift in movement above surface resulting from Earth’s spin
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Wind Coriolis Effect: Northern Hemisphere – Shift is always to the RIGHT
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Wind Coriolis Effect: Northern Hemisphere – Shift is always to the RIGHT Southern Hemisphere – Shift is always to the LEFT
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Wind Coriolis Effect:
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Wind Global Wind Patterns:
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Humidity Moisture in the air ( water vapor )
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Humidity Moisture in the air ( water vapor ) Relative Humidity – a measure of the amount of moisture % RH = moisture in air Moisture air can hold
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Humidity Psychrometer – instrument with a dry and wet bulb used to measure relative humidity
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Clouds Collection of condensed moisture in the air (moisture condenses to dust particles)
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Clouds 3 Types of Clouds:
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Clouds 3 Types of Clouds: 1. Cumulus – white, tall and fluffy
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Clouds 3 Types of Clouds: 2. Stratus – grey, flat and layered
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Clouds 3 Types of Clouds: 3. Cirrus – feathery, high + wispy
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Precipitation Rain Snow Sleet Hail Freezing rain Acid Rain
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Weather Forcasting Weather map symbols Buy’s Ballots Law Orographic Effect
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Climate General weather in an area over a long period of time
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