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CH 15 – Air, Weather, Climate
Pages: 323 – 329; + Inconvenient Truth
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Patterns?
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F
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Weather or Climate? Weather: short-term atmospheric events at a specific locality Climate:
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Weather: short-term atmospheric events at a specific locality
Climate: long-term patterns of weather over broad regions
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Weather and climate in middle GA?
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Weather and climate in middle GA?
warm, humid summers (thunderstorms) long growing season mild winters rainfall - winter
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The sun is the climate engine
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Infrared radiation derived from sunlight is the climate engine
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Weather and Climate the result of
solar radiation ambient temperature
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Weather and Climate the result of
solar radiation ambient temperature Moisture (evaporation and transpiration) Wind (transfer of mass between low and high pressures)
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Basic atmospheric structure
Stratosphere – km Troposphere – 0-10 km Basic atmospheric structure
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Structure of atmosphere
limited water vapor Weather and Climate constrained by atmosphere
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Structure of atmosphere
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4 principles of Climate curvature tilt
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A hypothetical continent
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4 principles of Climate 1. The sun heats unevenly. curvature tilt
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Solar Radiation heats the earth (unevenly)
Sun’s rays Atmosphere Large surface area 40% insolation at poles compared to tropics Small surface area Equator Earth
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angle of sunlight UNlabeled
Consider the Equinox solar equator = latitudinal equator
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40 Clouds and rainfall keep temperature uniform across the tropics 30 20 10 Mean annual temperature °C -10 -20 10 20 30 40 50 60 70 80 Degrees latitude
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The angle of the earth’s axis is responsible for seasonal variations on the earth.
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angle of sunlight UNlabeled
Consider the Equinox solar equator = latitudinal equator
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22 September 21 March
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21 June
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21 December
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Solar equator shifts N and S
influencing rainfall
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Solar Equator Heated air rises, cools, releases rain
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Relationship between solar energy and rainfall?
relative humidity
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relative humidity Water evaporates heated, moisture-laden air rises
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relative humidity air pressure and temperature drop
rising air expands and cools
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relative humidity Relationship between solar energy and rainfall?
5. Condensation begins (moisture holding capacity decreases) 6. precipitation may result
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Solar Equator Heated air rises, cools, releases rain Low pressure at surface (Tropical Lows) surface air moves in from North and South
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30 N & S of solar equator Cooled air sinks, warms, ‘holds more’ moisture
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30 N & S of solar equator Cooled air sinks, warms, picks up moisture High pressure at surface deserts in the Horse Latitudes
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development of a Hadley cell
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all three hadley flow and winds
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1. Solar Radiation heats the earth (unevenly)
latitudinal gradients in temperature Hadley cells determine distribution of rainfall and pressure tropical lows, subtropical highs Major forest types and deserts
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Biomes
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2. The Earth Spins Speed at North Pole? Equator?
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The Earth spins ‘The Coriolis Effect’ Predominant Winds
Tropical easterlies (0-30º) Temperate westerlies (30º-60º)
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Hurricane Season ITCZ
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Climate 3. Wind pushes water creating gyres
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Wind pushes Water Nova Scotia - England
Ocean currents distribute energy and modify coastal climates
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Driest deserts in the world lie on the west coasts of continents
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Annual World Precipitation
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Regional Climatic Influences
Topography and Geography modify patterns generated by principles 1-3
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Regional Climatic Influences
Topography and Geography modify pattterns generated by principles 1-3 a. The Rain Shadow Effect b. Altitudinal Effects c. Continental effects (oceans mediate extremes)
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Regional Climatic Influences
Pacific NW – Olympic and Cascade mtn ranges The Rain Shadow Effect
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Temperate “Rainforests”
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Eastern Oregon dry grasslands
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e.g. rain shadow in N. A. North American Deserts
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Regional Climatic Influences
Topography and Geography modify pattterns generated by principles 1-3 a. The Rain Shadow Effect b. Altitudinal Effects c. Continental effects (oceans mediate extremes)
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Altitudinal Effects e.g., Cloud Forest biome of Trinidad
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Altitudinal Effects Even a few hundred meters can significantly alter community type.
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year-round 100% humidity
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Regional Climatic Influences
Topography and Geography modify pattterns generated by principles 1-3 a. The Rain Shadow Effect b. Altitudinal Effects c. Continental effects (interiors experience temperature extremes)
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Variation in Climate Determines distribution of large scale assemblages of organisms
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A hypothetical continent
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