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[world-cruising] Coriolis effect

From: David Straton (no email)
Date: Wed Mar 15 2006 - 16:02:14 EST

  • Next message: Nancy Birnbaum: "[world-cruising] Re: Transporting boat question"

    Hi cruisers,

    I am trying to get my head around meteorology, and as part of it I have
    been making notes in the form of a web page. Its going quite well, but
    there's a long way to go.

    I have struck a problem explaining the Coriolis effect, and I thought
    some people on this list might be able to help.

    The basic rule of the Coriolis effect is that on a rotating sphere, a
    moving object tends to swerve to the right in the northern hemisphere,
    and to the left in the southern hemisphere. I can explain this well for
    objects moving north, south and east, but my explanation comes up with
    the answer that objects moving west should swerve towards the equator,
    thus left in the northern hemisphere. Thus my explanation must be wrong,
    I think.

    If this interests anyone out there, please put me right.

    The incomplete website is
    http://www.psyberspace.com.au/Cruising/meteorology.htm

    The text of it is below.

    Cheers

    Dave
    ------------------------------------------------------------------------

    Coriolis Effect

    One way I have found helpful to think of the Coriolis effect is to
    imagine the Earth as consisting of two nine-lane motorways, one in the
    northern hemisphere and one in the southern.

    Whereas the meridians of longitude are all the same length (approx
    40,000km), the parallels of latitude vary.

    Since the Earth rotates once every 24 hours, it follows that the
    rotational speed in km/h varies with different latitudes.

    http://www.psyberspace.com.au/Cruising/Images/DegreLongitude.gif

    Latitude
        
     At the north pole, Length of 1° longitude. (Km) = 0. Speed = 0 km/h
     At 80°, Length of 1° longitude. (Km) = 19. Speed = 291 km/h
     At 70°, Length of 1° longitude. (Km) = 39. Speed = 573 km/h
     At 60°, Length of 1° longitude. (Km) = 56. Speed = 837 km/h
     At 50°, Length of 1° longitude. (Km) = 72. Speed = 1,075 km/h
     At 40°, Length of 1° longitude. (Km) = 85. Speed = 1,281 km/h
     At 30°, Length of 1° longitude. (Km) = 96. Speed = 1,447 km/h
     At 20°, Length of 1° longitude. (Km) = 105. Speed = 1,570 km/h
    At 10°, Length of 1° longitude. (Km) = 110. Speed = 1,644 km/h
    At the Equator, Length of 1° longitude. (Km) = 111. Speed = 1,670 km/h
        
    So imagine yourself in the outside lane of this 9-lane motorway, on the
    Equator, hooning along in an easterly direction at 1,670 km/h. The car
    in the lane inside you, in the northern hemisphere, is going slower, and
    the ones inside that, slower still. Now imagine trying to throw a tennis
    ball from one car to another. You throw it directly out of the window,
    at 90° to your direction of travel. The ball has your easterly velocity,
    so tends to pass in front of the car inside you. It appears to swerve to
    the right, or to the east.

    A ball thrown from a car in one of the slower tracks to a faster car
    appears to swerve to the right, or the west, and pass behind the faster
    car.

    http://www.psyberspace.com.au/Cruising/Images/coriolis1.GIF

    The Coriolis effect is a little more difficult to explain for objects
    moving in an east-west direction. Imagine throwing your tennis ball
    directly east from your moving car on the 40° northern parallel. Your
    car continues round the track, a 'small circle' with its centre a point
    on the axis of the Earth's rotation, between the equatorial plane and
    the Pole. The ball continues its tangent from where you threw it, but
    follows a 'great circle' determined by gravity operating towards the
    centre of the Earth, on the equatorial plane. To you, in your speeding
    car, the ball appears to veer to the right.

    Thus, when wind rushes from a high pressure zone towards a lower
    pressure, in the northern hemisphere it tends to swerve right, and get
    into an anticlockwise spiral.

    http://www.psyberspace.com.au/Cruising/Images/coriolis2.GIF

    See this anti-clockwise Low Pressure system in the northern hemisphere.

    http://www.psyberspace.com.au/Cruising/Images/692px-Low_pressure_system_over_Iceland.jpg

    Depression over Iceland

    The opposite occurs in the southern hemisphere, with the Coriolis effect
    causing wind direction to bend leftwards, and depressions or cyclones to
    rotate in clockwise direction.

    Southern Hemisphere cyclone

    http://www.psyberspace.com.au/Cruising/Images/cyclone_lrg.jpg

    Cyclone Fay over Western Australia on March 25, 2004.

    Buys-Ballot Rule in the Southern Hemisphere says: 'If you LOOK into the
    wind, the LOW is on your LEFT.'

     
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