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    Institute of Meteorology and Geophysics , Karachi , Pakistan

    S tudents

    C loud

    O bservations

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    The CERESExperiment:

    Question:

    What is the Effectof Cloudson theEarths Climate?

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    Global Cloud Cover: 50-70%

    is soimportant

    about a few

    Clouds in

    the Sky?

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    How do

    clouds

    transmit

    and/or

    reflect

    radiation?__________

    Do clouds

    cool down

    or heat up

    the Earths

    climate?

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    Remote Sensing

    Remote sensing has been defined as "a technique usedto gather information about an object or an area without actually

    touching it. Our eyes, ears, and skin, as well as more sophisticated

    instruments, all aid us in remote

    sensing.

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    Cloud Types and Levels

    Cloud Cover

    Visual Opacity

    (Percentage)

    (How much light penetrates the cloud)

    CUMULUS

    CIRRUS

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    Do you have any CLOUD

    EXPERIENCE?Well, I have looked at clouds in the sky since I was a little

    kid. One time I saw a cloud that looked like.

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    Any other experience with clouds?

    I cant think of any, Im in a FOG.

    Thats it! Yes, Ive been in a CLOUD.

    Ive walked through FOG

    (a cloud formed near the ground)

    Lets get out of this fog and move into clearer visibility.

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    Necessary Ingredients:

    Hygroscopic nuclei consist of particles such as

    sea salt which have an affinity (attraction) for

    water. Water vapor condenses on these particles.

    WATER (vapor)

    CHANGE INTEMPERATURE

    (cooler)

    CONDENSATIONNUCLEI (aerosols)

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    Just over 200 years ago (in 1803),

    Luke Howard used Latin words to

    name the cloud types.

    Cumulusmeans pile and describes heaped, lumpy cloudsCirrusmeans hair and describes wispy looking clouds.

    This term is also used to describe high level clouds

    Stratusmeans layer and describes clouds that form in

    sheets and do not have any unique features

    Cumulusmeans pile and describes heaped, lumpy clouds

    Cirrusmeans hair and describes wispy looking clouds.

    This term is also used to describe high level clouds

    Stratusmeans layer and describes clouds that form in

    sheets and do not have any unique features

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    Nimbusmeans rain and describes low grey rain clouds

    Altodescribes mid level clouds

    Cumuluslumpy Cirruswispy Stratus - layered

    Contrailsshort for condensation

    trails are the only man-made cloud

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    Cumuluslumpy Cirruswispy Stratuslayered

    Nimbusraining Altomid-level Contrails - streaks

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    Cumuluslumpy Cirruswispy Stratuslayered

    Nimbusraining Altomid-level Contrails - streaks

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    Cumuluslumpy Cirruswispy Stratuslayered

    Nimbusraining Altomid-level Contrails - streaks

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    Cumuluslumpy Cirruswispy Stratuslayered

    Nimbusraining Altomid-level Contrails - streaks

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    Imagine that you are

    looking through a window.

    Notice the dark grey patches on the cloudslack of light.

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    Note the silhouette of the sunthere is some

    light penetrating through the cloud cover.

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    Note the clear outline seen of the sun despite

    the cloud cover.

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    LETS OBSERVE!

    Lets make an

    observation

    on what we

    see on this

    beautiful day!

    What cloud

    types are

    present?

    Whats the

    percentage of

    cloud cover?

    How much

    light

    penetrates

    the clouds?

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    CLOUD CLASSIFICATION

    THE 27 STATES OF SKY

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    LOW CLOUDS

    POLAR REGIONSSurface - 6,500 ft

    Surface - 1,981 m

    TEMPERATE REGIONSSurface - 6,500 ft

    Surface - 1,981 m

    TROPICAL REGIONSSurface - 6,500 ft

    Surface - 1,981 m

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    LOW CLOUDS

    CL= 1

    Cumulus of little vertical development, or ragged cumulus.

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    LOW CLOUDS

    CL = 2

    Towering cumulus (TCU): Cumulus of moderate or greater vertical development

    LOW CLOUDS

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    LOW CLOUDS

    CL= 3

    Cumulonimbus (Cb) -- Cumulus of great vertical development (no cirrus anvil)

    LOW CLOUDS

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    LOW CLOUDS

    CL= 4

    Stratocumulus (Sc) formed by the spreading of cumulus

    LOW CLOUDS

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    LOW CLOUDS

    CL= 5

    Stratocumulus (SC) notformed by the spreading of cumulus

    LOW CLOUDS

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    LOW CLOUDS

    CL= 6

    Stratus (St) in a relatively continuous layer, or ragged shreds (other

    than that of bad weather), or both

    LOW CLOUDS

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    LOW CLOUDS

    CL= 7

    Low clouds in the form of stratus fractus (StFRA), cumulus fractus (CuFRA), or

    both, usually below altostratus (As) or nimbostratus (Ns).

    LOW CLOUDS

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    LOW CLOUDS

    CL= 8

    Cumulus (Cu) and stratocumulus (Sc; notformed by the spreading of cumulus)

    with bases at different levels

    LOW CLOUDS

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    LOW CLOUDS

    CL = 9

    Cumulonimbus (Cb), where the upper part of at least one of the (Cb) clouds in clearly

    fibrous or striated. By convention, code figure 9 is used for Cumulonimbus Mammatus

    (CbMAM) and those cases in which lightning, thunder, or hail indicates the presence of a

    Cb but the top is hidden by darkness or other clouds

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    MIDDLE CLODS

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    MIDDLE CLODS

    CM= 1

    Altostratus (As): Predominantly transparent or semitransparent

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    MIDDLE CLODS

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    MIDDLE CLODS

    CM = 4

    Altocumulus standing lenticular (AcSL): AC in the form of semitransparent

    patches (often fish-shaped, almond-shaped, or lenticular) continuously

    changing in appearance and occurring at one or more levels

    MIDDLE CLODS

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    MIDDLE CLODS

    CM= 5

    Altocumulus (Ac) progressively invading the sky

    MIDDLE CLODS

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    MIDDLE CLODS

    CM= 6

    Altocumulus (Ac) formed by the spreading or flattening of Cu or Cb

    MIDDLE CLODS

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    CM= 7Altocumulus (Ac) at two or more levels, not progressively invading the

    sky; or, opaque Ac at one level, not progressively invading the sky; or,

    altostratus (As) or nimbostratus together with Ac.

    (Note: This code is generally used as a catch-all by weather observers)

    MIDDLE CLODS

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    CM = 8

    Altocumulus Castellanus (AcC): Altocumulus in the form of turrets or battlements or

    AC having the appearance of small cumuliform tufts, with or without altostratus (As)

    or nimbostratus (Ns)

    MIDDLE CLODS

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    CM= 9

    Altocumulus (AC) of a chaotic sky, with or without altostratus (AS) or

    nimbostratus (NS).

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    HIGH CLOUDS

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    HIGH CLOUDS

    CH= 1

    Cirrus (Ci) in the form of thin filaments, strands, or hooks (not

    progressively invading the sky)

    HIGH CLOUDS

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    HIGH CLOUDS

    CH= 2

    Cirrus (Ci) in predominantly dense patches or with sproutings in the form of small tufts

    or battlements

    HIGH CLOUDS

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    HIGH CLOUDS

    CH = 3

    Dense cirrus (Ci) (often in the form of an anvil) originating from cumulonimbus (Cb)

    HIGH CLOUDS

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    G C OU S

    CH= 4

    Cirrus (Ci) in the form of hooks, filaments, or strands, invading the sky

    and generally growing denser

    HIGH CLOUDS

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    CH= 5Cirrostratus (Cs) (with or without cirrus) progressively invading the sky, and the

    continuous veil extends 45 degrees or less above the local horizon

    HIGH CLOUDS

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    CH= 6

    Cirrostratus (Cs) (with or without cirrus) progressively invading the sky,

    and the continuous veil extends more than 45Oabove the local horizon

    but does not cover the whole sky

    HIGH CLOUDS

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    CH= 7

    Cirrostratus (Cs) covers the entire sky. (Note: The example shown here

    also includes condensation trails, or contrails.)

    HIGH CLOUDS

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    CH= 8

    Cirrostratus (CS) doesnot cover the entire sky

    and is not invading the

    celestial dome

    HIGH CLOUDS

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    CH= 9

    Cirrocumulus (Cc) alone, or predominant when compared with combined sky

    cover of any cirrus (Ci) or cirrostratus (Cs) present