Climate and Climate Change Environmental Science Spring 2011.
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Transcript of Climate and Climate Change Environmental Science Spring 2011.
![Page 1: Climate and Climate Change Environmental Science Spring 2011.](https://reader035.fdocuments.us/reader035/viewer/2022070401/56649f1b5503460f94c3013c/html5/thumbnails/1.jpg)
Climate and Climate Change
Environmental ScienceSpring 2011
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ObjectivesExplain the difference between weather and
climate Identify four factors that determine climate Explain why different parts of the Earth have
different climates Explain what causes the seasons
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Weather and ClimateWeather: is the state of the atmosphere at a
particular place at a particular moment Climate: is the long-term prevailing weather
conditions at a particular place based upon records taken
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Weather and ClimatePhoenix, AZ and Seattle, WA may have the
same weather on a particular day (may be warm in both places), but climates are quite different (Phoenix is hot and dry, Seattle is cool and moist)
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Factors Determining ClimateLatitude
Most important is distance from equator Atmospheric circulation patternsOceanic circulation patterns Local geography of an area Solar activity Volcanic activity
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LatitudeLatitude: the distance from the equator
measured in degrees north or south of the equator
Equator: located at zero degrees latitudeNorth Pole: most northerly latitude, 90
degrees northSouth Pole: most southerly latitude, 90
degrees south
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LatitudeLatitude influences climate because the
amount of solar energy an area of Earth receives depends on its latitude
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LatitudeLow latitude
More solar energy falls on areas that are near equator
Incoming solar energy is concentrated on a relatively small surface area at the equator
In areas near equator night and day are about 12 hours long throughout the year
Temperatures are high year round, no summers or winters
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LatitudeHigh latitude
In regions close to poles, amount of energy arriving at surface is reduced
In northern and southern latitudes, sunlight hits Earth at oblique angle and spreads over a larger surface area
Average temperatures are lowerHours of daylight vary
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Atmospheric Circulation Air circulation affects climate
Cold air sinks because it is denser than warm air As cold air sinks, it compresses and gets warmer
Warm air rises Expands and cools as it rises
Warm air can hold more water vapor than cold air can When warm air cools, the water vapor it contains
may condense (rain)
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Atmospheric Circulation
Wind: the movement of air within atmosphere
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Atmospheric Circulation Because Earth rotates, and because different
latitudes receive different amounts of solar energy, pattern of global atmospheric circulation results Determines Earth’s precipitation pattern
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Global Circulation PatternsCool air over equator cannot sink because
hot air is rising below it Cool air rises and is forced away from the
equator
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Global Circulation PatternsAt about 30 degrees north and south latitude,
some of cool air sinks, becomes warmer as sinks
Warm, dry air moves across land and causes water to evaporate from land below, which creates dry conditions
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Global Circulation PatternsAt about 60 degrees north and south latitude,
air collides with cold air traveling from poles Warm air risesWhen rising air reaches top of troposphere,
small amounts return back to circulation patterns between 60 and 30 degrees north and south latitude
Most of uplifted air is forced toward polesCold dry air descends at poles (cold deserts)
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Prevailing WindsPrevailing winds: winds that blow in mostly
one direction throughout the year Because of rotation of Earth, deflected to the
right in the Northern hemisphere and to the left in the Southern hemisphere
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Prevailing WindsTrade Winds: belts of prevailing winds
between 30 degrees north and south latitudes and the equator Blow from the northeast in Northern
hemisphere and southeast in the Southern hemisphere
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Prevailing WindsWesterlies: produced between 30 and 60
degrees north and south latitudes Northern hemisphere these westerlies are
southwest winds Southern hemisphere these westerlies are
northwest winds
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Prevailing WindsPolar Easterlies: blow from poles to 60
degrees north and south latitudes
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Oceanic Circulation Patterns Movement of surface ocean currents is
caused mostly by winds and rotation of Earth Redistribute warm and cool masses of water
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Oceanic Circulation Patterns El Nino- Southern Oscillation
El Nino and La Nina are opposite phases of ENSOEl Nino warmer phase, La Nina colder phase
El NinoShort term (6-18 months) periodic change in
location of warm and cold water masses in the Pacific Ocean
Warm water pushed eastward Increased rainfall eastward (southern half of US)
La NinaWater in the eastern Pacific Ocean is cooler than
usual
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Oceanic Circulation Patterns Pacific Decadal Oscillation
Long term, 20 to 30 year change in location of warm and cold water masses in Pacific Ocean
Influences climate in northern Pacific Ocean and North America
Affects ocean surface temperatures, air temperatures, and precipitation patterns
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Topography Elevation effects climateTemperatures fall by about 6 degrees C for
every 11,000m increase in elevation
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Topography Mountains and mountain ranges influence
distribution of precipitation Sierra Nevada mountainsWhen warm air hits mountains it risesAs air rises, it cools, which causes rain on
western side of mountains By the time air reaches eastern side of
mountains, it is dryRain shadow effect
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Other Influences on Earth’s Climate Solar maximum: sun emits an increased
amount of UV radiation UV produces more ozone, warming the
stratosphere Increased radiation can also warm the lower
atmosphere and surface of the Earth a little
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Other Influences on Earth’s Climate Large scale volcanic eruptions
Sulfur dioxide gas can reach the upper atmosphere
Sulfur dioxide reacts with smaller amounts of water vapor and dust in stratosphere
Reaction forms a bright layer of haze that reflects enough sunlight to cause global temperature to decrease
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Seasonal Changes in Climate Seasons result from tilt of Earth’s axis (about
23.5 degrees relative to the plane of its orbit)Because of tilt, the angle at which the sun’s
rays strike the Earth changes as the Earth moves around the sun
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Seasonal Changes in Climate During summer in Northern Hemisphere, the
Northern Hemisphere tilts toward the sun and receives direct sunlight Number of daylight is greatest
During summer in Northern Hemisphere, the Southern Hemisphere tilts away from the sun and receives less direct sunlight
During summer in Southern Hemisphere, situation is reversed Southern Hemisphere tilted toward sun,
Northern hemisphere tilted away