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    GROUP 4

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    PRINCIPLESOF

    ANEROID

    BAROMETER

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    Aneroid barometeris an

    instrument

    measuring atmospheric pressure

    invented by French scientist Lucien

    Vidie. It is constructed on the

    following principles:

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    Parts of an Aneroid Barometer

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    Principles of Mercurial Barometer

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    A mercury barometer has a

    glass tube with a height of at

    least 84 cm, closed at one

    end, with an open mercury-filled reservoir at the base.

    Invented by Evangelista

    Toricilli

    The weight of the mercury

    creates a vacuum in the top

    of the tube. Mercury in the

    tube adjusts until the weightof the mercury column

    balances the atmospheric

    force exerted on the

    reservoir.

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    High atmospheric pressure places more forceon the reservoir, forcing mercury higher in thecolumn.

    Low pressure allows the mercury to drop to a

    lower level in the column by lowering theforce placed on the reservoir.

    Since higher temperature at the instrument

    will reduce the density of the mercury, thescale for reading the height of the mercury isadjusted to compensate for this effect.

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    DISTINGUISHTHEATMOSPHERIC

    PRESSUREREADINGOF ANEROIDBAROMETERANDTEMPERATURE

    READING.

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    To read your barometer, first tap the

    glass lightly, but firmly, to ensure that

    the linkage mechanism is not sticking.

    The hectopascal is the international

    meteorological unit of pressure. One

    hectopascal is exactly equal to onemillibar, the unit of pressure mainly

    used for barometer scales before

    1986.

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    The other hand that is found on

    most instruments is the 'setpointer' (usually brass). This can

    be turned by means of the knob

    at the centre of the glass so that itcovers the reading pointer. In this

    way you can tell, next time you

    check your barometer, whether

    the pressure is now lower or

    higher and by how much.

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    STATE THE FUNCTIONS OF

    HYGROMETER AND EXPLAINTHEIR BASIC PRINCIPLES

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    Hygrometer

    Instrument used in finding the Dew - point

    temperature .

    It is always accompanied by a table which

    shows the difference in dew point between

    the dry-bulb temperature and the wet-bulb

    temperature

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    Example :

    Dry bulb temperature (t) = 20.8C

    Wet bulb temperature (t) = 19.4CCalculations:

    you get t-t = 1.4 and t=19.4. In the table, you

    can find:

    Dew point temperature = 19.0 for t-t-1.0 and t-19.5(the

    nearest value for 19.4)

    Dew point temperature = 18.8 for t-t= 1.5 and t = 19.5.

    then make the interpolation to get the dew-point

    temperature for t-t = 1.4 and t = 19.5

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    19.0+ (18.8-19.0)(1.4-1.0)/(1.5-1.0) = 18.8

    Finally , make the interpolation to get the dew

    point temperature for t-t = 1.4 and t = 19.4assuming the variance of t is approximately

    the same with 18.8 0.1 = 19.7C