Bio 126 Climate and Weather

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Bio 126 Bio 126 Climate and Weather Climate and Weather

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Bio 126 Climate and Weather. Earth from the moon. Meteorology. Climate- over all combination of temperature and precipitation that a region experiences Mediterranean= winter precipitation followed by long hot, dry summers Weather- daily, weekly variations in these phenomena. - PowerPoint PPT Presentation

Transcript of Bio 126 Climate and Weather

Page 1: Bio 126 Climate and Weather

Bio 126Bio 126Climate and WeatherClimate and Weather

Page 2: Bio 126 Climate and Weather

Earth from the moonEarth from the moon

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MeteorologyMeteorology

Climate- over all combination of temperature and precipitation that a region experiences– Mediterranean= winter precipitation

followed by long hot, dry summers Weather- daily, weekly variations in

these phenomena

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Solar radiationSolar radiation

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Climate zonesClimate zones

Warm at equator, cooler towards poles.– Caused by intensity of sunlight at

equator.– Poles receive less on a per area basis.

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Solar radiation around the Globe

Solar radiation around the Globe

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SeasonsSeasons

Caused by tilting of earth on its rotational axis.– Intensity of sunlight varies.– Most extreme at poles– Little change at equator.

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Causes of SeasonsCauses of Seasons

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PrecipitationPrecipitation

Varies by latitude.Wet at equator 00, and 600 N / SDry at 300, and 900 poles

– Poles are frozen desertsCaused by formation of Hadley Cells

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Hadley CellsHadley Cells

Air currents in Hadley Cells caused by air density not just temperature.

Uneven heating in different regions on the earth cause winds.

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Hadley CellsHadley Cells

Air rises (0, 60) due to warming of surface.

– Adiabatic Cooling as air rises as rises the air becomes less dense and cooler this cause water to condense and fall as rain, snow

Air falls (30, poles) – Adiabatic warming as air falls

air becomes compressed, and heats. air absorbs moisture, falls as dry air and absorbs

moisture from the environment.

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Global air circulation, precipitation, and winds: Hadley cellsGlobal air circulation, precipitation, and winds: Hadley cells

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Global Air CirculationGlobal Air Circulation

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West Coast LatitudesWest Coast Latitudes

San Diego=32.5; LA= 34; Sta. Barbara= 34.5 ; Sta. Cruz=37, SF 37.75; Eureka= 40.75

Approx. Portland= 45.5; Seattle= 47.5 ; Juneau= 58; Anchorage = 61

CA large enough to span climate zones between Hadley cells.

– South dry– North wet

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Seasons- Seasons-

tilting of earth moves solar equator. Effectively moves 300 dry zone

north in summer– descending dry air belt is pushed

farther north in our summer, the wet belt moves farther south

giving us wet winters

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Causes of SeasonsCauses of Seasons

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Prevailing windsPrevailing winds

These Hadley cell wind currents move North or South

The spinning of the earth makes it seem like they come at an angle.– In CA our winds, storms usually come

from the south west.– Rains often bring warmer weather

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Ocean currentsOcean currents Prevailing winds cause ocean waters to

move in the prevailing direction. huge gyres form due to earth’s spinning

known as the Coriolus effect – In Northern Pacific clockwise general

direction of flow from our coast.– Ca. Current, with its cold, nutrient rich water

flows from Alaska southwards along our coast

– At Sta. Barbara coastline moves east, current flows due south, allowing Southern Ca. water to warm

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Hadley cellsHadley cells

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Barometer measures air Barometer measures air pressure pressure

Low pressure (rising air) associated with storms.

High pressure (descending air) blocks storms.

– High pressure off California in summer blocks most storms

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Global Trade Wind PatternsGlobal Trade Wind Patterns

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Ocean CurrentsOcean Currents

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BiomesBiomes

Major vegetation types that also determine the animal community present.

Determined mostly by climate – Soil also important factor

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Figure 50.3 A climograph for some major kinds of ecosystems (biomes) in Figure 50.3 A climograph for some major kinds of ecosystems (biomes) in North AmericaNorth America

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BiomesBiomes

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Patterns of distribution in the biospherePatterns of distribution in the biosphere

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Major BiomesMajor Biomes

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Coniferous forest, Lady Bird Grove (top left), Sequoias (right), rain forest Coniferous forest, Lady Bird Grove (top left), Sequoias (right), rain forest (bottom left)(bottom left)

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Temperate deciduous forest, Great Smokey Mountains National ParkTemperate deciduous forest, Great Smokey Mountains National Park

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Tropical forestsTropical forests

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SavannaSavanna

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Desert. Organ Pipe State Park (top), Joshua Tree National Park (bottom left), Death Desert. Organ Pipe State Park (top), Joshua Tree National Park (bottom left), Death Valley (bottom right)Valley (bottom right)

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Temperate grassland- PrairieTemperate grassland- Prairie

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Tundra. Denali National Park (left), reindeer (right)Tundra. Denali National Park (left), reindeer (right)

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Rain shadow Rain shadow Precipitation increases as storms

are pushed up over mountians.– accordingly rain becomes snow

– As air moves up slope in the Sierras it cools 3-5 degrees per 1,000 ft.

This is the same effect as moving 300 miles farther north !

Causes deserts in Nevada

Most islands with mountains have wet and dry sides

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RainshadowRainshadow

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RainshadowRainshadow

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Summer Fog Summer Fog

– Inland air warms quickly. This rising air, pulls in coastal air.

– Cold water off CA. cools incoming warm, moist ocean

– Coast causes summer fog. Essential for southern ranges of

Coast Redwoods, and relic pines, cypress species

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Temperature Inversion layersTemperature Inversion layers

dense air flows downhill and collects in low spots, valleys. Great Central valley is an example.

– This dense air may be blocked by hills etc. from warmer winds which blow over the top of dense air, leaving it alone.

– Dense tule fog may form for days. Inversion layer (cold air higher up) also traps

pollutants. Mexico City problems Reno, Tahoe now ban fireplaces.

Often “burn off” in summer but leave the haze of phytochemical smog behind.

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