Climate and Weather

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Climate and Weather Climate and Weather ISCI 2001

description

Climate and Weather. ISCI 2001. Climate and Weather. Climate Zones. The Earth’s Atmospheres. Mostly nitrogen (78%) and oxygen (21%) Troposphere Temperature -50 to 40 Celsius Stratosphere Ozone layer (O 3 ) UV light. Greenhouse Effect. - PowerPoint PPT Presentation

Transcript of Climate and Weather

Page 1: Climate and Weather

Climate and Weather Climate and Weather ISCI 2001

Page 2: Climate and Weather

Climate and Weather Climate and Weather

Page 3: Climate and Weather

Climate Zones Climate Zones

Page 4: Climate and Weather

The Earth’s Atmospheres The Earth’s Atmospheres Mostly nitrogen (78%) and oxygen

(21%)◦Troposphere

Temperature ◦-50 to 40 Celsius

Stratosphere ◦Ozone layer (O3)

◦UV light

Page 5: Climate and Weather

Greenhouse Effect Greenhouse Effect Terrestrial radiation ‘trapped’ by

greenhouse gases◦Carbon dioxide

Page 6: Climate and Weather

Greenhouse Effect – Greenhouse Effect – Greenhouse Gases Greenhouse Gases • (1). Carbon dioxide

– Fossil fuels; deforestation; organic decay; forest fires

• (2). Ozone– Sunlight chemically reacts with O2 (natural)– Photochemical smog production

• (3). Methane– Wetlands; biomass burning; termites; organic decay

• (4). Chlorofluorocarbons– Refrigerants; aerosol spray propellants; cleaning solvents

• (5). Nitrous Oxide – Fertilizers; burning of fossil fuels; forests; grasslands

Page 7: Climate and Weather

Importance of Ozone Importance of Ozone Absorbs UV radiation

Formed in the stratosphere

Chlorofluorocarbons (CFCs)

Ozone Holes

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GH Effect Importance GH Effect Importance Naturally warms the surface of

the Earth

Keeps the average temperature of the Earth normal (sustain life)◦-18 C otherwise

Global Warming ◦Increased GH effect, GH gases

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Atmospheric PressureAtmospheric PressureDensity of air decreases with altitude

◦‘thinning’ of air

Sea Level ◦1cubic meter

Mass 1.2 kg (at 10 km 0.4 kg)

101.3 kPa or 1 atmosphere of pressure

Barometer

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Atmospheric Pressure Atmospheric Pressure

Page 11: Climate and Weather

How Winds are produced How Winds are produced Air that flows from high to low pressure

areas◦ Uneven heat of the Earth’s surface

Warm air is lower density and low air pressure Cool air higher density and higher air pressure Isobars

Produces a convection current

Local winds ◦ Small scale changes in convection cells and

pressure gradients ◦ Global wind patterns – prevailing winds

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Winds – Convection Cells Winds – Convection Cells

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Prevailing Winds – Hadley Prevailing Winds – Hadley Cells Cells

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Coriolis Effect Coriolis Effect Earth Rotation effects global wind

patterns ◦Objects deviate from straight-line

path including winds – deflected

Deflects winds to the right in the Northern Hemisphere and to the Left in the Southern Hemisphere

Jet Streams

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Cloud Formation and Cloud Formation and PrecipitationPrecipitationAggregates of water droplets

formed by rising air that expands and cools ◦Cumulus, stratus or cirrus

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Cloud Classification Cloud Classification

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Cirrocumulus

Cirrostratus

Altocumulus

Cumulonimbus

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Air Masses and Fronts Air Masses and Fronts Air Mass

◦Arctic, polar, tropical

Weather Fronts ◦Warm vs Cold Fronts ◦Stationary

Animation

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Fronts Fronts

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Formation of Cyclones Formation of Cyclones Hurricanes

Tornados

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Solar Radiation, Tilting of the Solar Radiation, Tilting of the Earth and the Seasons Earth and the Seasons