1-the origin of winds

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    Climate Change. ITESM

    Campus Saltillo.

    Flavio Orta-Dvila

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    Wind is the movement (usuallyhorizontal) of air in the atmosphere

    Wind is caused by a difference in thetemperature between different regions ofthe earth.

    This temperature between different airlayers occurs mainly because of theheating of the earths surface by the sun.

    Thus, the air above these surfaces absorbsdifferent amounts of heat. Making it warmin places and cool in others.

    The greaterthe difference, the fasterthe wind moves

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    Air Pressure

    Differences in air pressure

    are caused by the unevenheatingof Earth

    Uneven heating producespressure beltswhich

    occur every 30 latitude

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    What is the Albedo Effect?

    Albedoor reflection coefficient, derivedfrom Latinalbedo"whiteness" (orreflected sunlight) in turn from albus"white," is the diffuse reflectivityor

    reflecting power of a surface. It is the ratio of reflected radiation from

    the surface to incident radiation upon it.

    It is expressed in percentage (being closezero a black surface, and a high number awhite perfect reflection (like ice).

    http://en.wikipedia.org/wiki/Latinhttp://en.wikipedia.org/wiki/Diffuse_reflectionhttp://en.wikipedia.org/wiki/Diffuse_reflectionhttp://en.wikipedia.org/wiki/Latin
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    Albedo Effect

    Albedo depends on the frequencyof theradiation (across the spectrum of visible light)

    The albedo is an important concept inclimatology, astronomy, and calculatingreflectivityof surfaces in LEEDsustainable-rating systems for buildings. The averageoverall albedo of Earth, its planetary albedo,

    is 30 to 35% because of cloud cover, butwidely varies locally across the surfacebecause of different geological and

    environmental features.

    http://en.wikipedia.org/wiki/Frequencyhttp://en.wikipedia.org/wiki/Visible_lighthttp://en.wikipedia.org/wiki/Climatologyhttp://en.wikipedia.org/wiki/Astronomyhttp://en.wikipedia.org/wiki/Reflectivityhttp://en.wikipedia.org/wiki/Leadership_in_Energy_and_Environmental_Designhttp://en.wikipedia.org/wiki/Leadership_in_Energy_and_Environmental_Designhttp://en.wikipedia.org/wiki/Reflectivityhttp://en.wikipedia.org/wiki/Astronomyhttp://en.wikipedia.org/wiki/Climatologyhttp://en.wikipedia.org/wiki/Visible_lighthttp://en.wikipedia.org/wiki/Frequency
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    ANEMOMETERThe speed of the wind

    is usually measured with this instrument.

    h f d

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    Characteristics of wind aredirection,speed

    The direction of wind is found out by aninstrument called the WIND VAN

    The speed of the wind is usually measuredwith an instrument calledANEMOMETER

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    ITCZ=Inter-tropicalClimate Zone.

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    Pressure Belts

    As warm airrises at the

    equator and moves towardthe poles, it cools

    As it cools, some of the airsinks around 30north

    and south of the equator

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    Pressure Belts

    At the poles, cold air

    sinksand movestowards the equator

    Around 60north andsouth, the air begins to

    heat u and rise

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    Global Winds

    The combination of pressure

    belts and the Coriolis Effectcause global winds

    These are polareasterlies, westerlies,

    and trade winds

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    Polar Easterlies

    Wind belts that extend from

    the poles to 60latitude

    Formed from cold sinking air

    moving from the polescreating cold

    temperatures

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    Westerlies (or Tropical Easterlies)

    Wind belts found between

    30and 60

    latitude

    Flow towards the poles

    from west to east carryingmoist airover the Unites

    States

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    Trade Winds

    Winds that blow from 30

    almost to the equator

    Called the trade windsbecause of their use by

    early sailorsNOTE: Alisos are known as Tradewinds predominantly high in summer,

    and slow in winter.They are associated withHardle Circulation cells.

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    Doldrums

    Located along the equator

    where no winds blowbecause the warm rising

    air creates and area oflow pressure

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    Horse Latitudes

    Occur at about 30north and

    south of the equator wherethe winds are very weak

    Most deserts on the Earth arelocated here because of thedry air

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    Jet Stream

    The jet streams are

    narrow belts of highspeed windsthat blowin the upper troposphere

    and lower stratosphereSeparateswarm air

    from cold air

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    Sea Breezes

    High pressure is created overthe ocean during the day andlow pressure over land due touneven heating

    Air moves from the ocean tothe land creating a seabreeze

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    Land Breezes

    Low pressure occurs over the

    ocean during the nightandhigh pressure over land due tothe uneven heating of earth

    This causes wind to move fromthe land to the ocean creating

    a land breeze

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    Question 1

    What causes winds?

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    Answer

    Winds are caused by the

    uneven heating ofEarths surface, which

    causes pressuredifferences

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    Question 2

    What are the three types

    of global winds?

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    Answer

    Polar Easterlies

    WesterliesTrade Winds

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    Question 3

    What is the difference

    between a land breezeand a sea breeze?

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    Answer

    Sea breezes occur during

    the day when the land iswarmer than water and a

    land breeze occurs atnight when the water is

    warmer than land

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    Here are some links of videosthat may help you understand:

    Wind circulation videohttps://www.youtube.com/watch?v=Ye45

    DGkqUkE Global Winds and Jet streams

    https://www.youtube.com/watch?v=j5x6y

    3a1eRs

    https://www.youtube.com/watch?v=Ye45DGkqUkEhttps://www.youtube.com/watch?v=Ye45DGkqUkEhttps://www.youtube.com/watch?v=j5x6y3a1eRshttps://www.youtube.com/watch?v=j5x6y3a1eRshttps://www.youtube.com/watch?v=j5x6y3a1eRshttps://www.youtube.com/watch?v=j5x6y3a1eRshttps://www.youtube.com/watch?v=Ye45DGkqUkEhttps://www.youtube.com/watch?v=Ye45DGkqUkE