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Husky Stadium Capacity Update

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Comments

  • section8section8 Member Posts: 1,581
    I like how they claim they didn't know he capacity, really? Pretty sure the architects could tell you.
  • DerekJohnsonDerekJohnson Administrator, Swaye's Wigwam Posts: 63,558 Founders Club
  • ApostleofGriefApostleofGrief Member Posts: 3,904
    edited August 2013

    New stadium guarantees extra wins, everyone says so.

    If the team can take advantage of atmospheric pressure caused by dropping the field elevation, new wins are guaranteed. Putting in the jumbotron was a stupid waste of money. What is needed is a barometer that coaches can access in real time. By that I mean that it would be better to have it digital (real time) than analog (subject to hysteresis). Read on:

    Atmospheric pressure is the force per unit area exerted on a surface by the weight of air above that surface in the atmosphere of Earth (or that of another planet). In most circumstances atmospheric pressure is closely approximated by the hydrostatic pressure caused by the weight of air above the measurement point. On a given plane, low-pressure areas have less atmospheric mass above their location, whereas high-pressure areas have more atmospheric mass above their location. Likewise, as elevation increases, there is less overlying atmospheric mass, so that atmospheric pressure decreases with increasing elevation. On average, a column of air one square centimeter in cross-section, measured from sea level to the top of the atmosphere, has a mass of about 1.03 kg and weight of about 10.1 N (2.28 lbf) (A column one square inch in cross-section would have a weight of about 14.7 lbs, or about 65.4 N).

    Atmospheric pressure based on height of water.

    Atmospheric pressure is often measured with a mercury barometer, and a height of approximately 760 millimetres (30 in) of mercury is often used to illustrate (and measure) atmospheric pressure. However, since mercury is not a substance that humans commonly come in contact with, water often provides a more intuitive way to visualize the pressure of one atmosphere.

    One atmosphere (101 kPa or 14.7 psi) is the amount of pressure that can lift water approximately 10.3 m (34 ft). Thus, a diver 10.3 m underwater experiences a pressure of about 2 atmospheres (1 atm of air plus 1 atm of water). This is also the maximum height to which a column of water can be drawn up by suction at atmospheric pressure.

    Low pressures such as natural gas lines are sometimes specified in inches of water, typically written as w.c. (water column) or W.G. (inches water gauge). A typical gas-using residential appliance is rated for a maximum of 14 w.c., which is approximately 35 hPa.

    In general, non-professional barometers are aneroid barometers or strain gauge based. See pressure measurement for a description of barometer

    http://en.wikipedia.org/wiki/Atmospheric_pressure

    It would be wise to use this formula in the game plan:

    http://upload.wikimedia.org/math/5/b/5/5b5cdd7bddb7a752110211845dfe3cf9.png
  • [Deleted User][Deleted User] Posts: 11,453

    New stadium guarantees extra wins, everyone says so.

    If the team can take advantage of atmospheric pressure caused by dropping the field elevation, new wins are guaranteed. Putting in the jumbotron was a stupid waste of money. What is needed is a barometer that coaches can access in real time. By that I mean that it would be better to have it digital (real time) than analog (subject to hysteresis). Read on:

    Atmospheric pressure is the force per unit area exerted on a surface by the weight of air above that surface in the atmosphere of Earth (or that of another planet). In most circumstances atmospheric pressure is closely approximated by the hydrostatic pressure caused by the weight of air above the measurement point. On a given plane, low-pressure areas have less atmospheric mass above their location, whereas high-pressure areas have more atmospheric mass above their location. Likewise, as elevation increases, there is less overlying atmospheric mass, so that atmospheric pressure decreases with increasing elevation. On average, a column of air one square centimeter in cross-section, measured from sea level to the top of the atmosphere, has a mass of about 1.03 kg and weight of about 10.1 N (2.28 lbf) (A column one square inch in cross-section would have a weight of about 14.7 lbs, or about 65.4 N).

    Atmospheric pressure based on height of water.

    Atmospheric pressure is often measured with a mercury barometer, and a height of approximately 760 millimetres (30 in) of mercury is often used to illustrate (and measure) atmospheric pressure. However, since mercury is not a substance that humans commonly come in contact with, water often provides a more intuitive way to visualize the pressure of one atmosphere.

    One atmosphere (101 kPa or 14.7 psi) is the amount of pressure that can lift water approximately 10.3 m (34 ft). Thus, a diver 10.3 m underwater experiences a pressure of about 2 atmospheres (1 atm of air plus 1 atm of water). This is also the maximum height to which a column of water can be drawn up by suction at atmospheric pressure.

    Low pressures such as natural gas lines are sometimes specified in inches of water, typically written as w.c. (water column) or W.G. (inches water gauge). A typical gas-using residential appliance is rated for a maximum of 14 w.c., which is approximately 35 hPa.

    In general, non-professional barometers are aneroid barometers or strain gauge based. See pressure measurement for a description of barometer

    http://en.wikipedia.org/wiki/Atmospheric_pressure
    Disagree
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