Difference between revisions of "Atmospheric pressure"

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'''Atmospheric pressure''' is also called the '''barometric pressure''' and varies with elevation above sea level. Also, at a given place it varies slightly from time to time because of changes in meteorological conditions.
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[[File:Atmospheric pressure mb heights.jpg|thumb|200px]]
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[[File:Atmospheric Pressure.jpeg|thumb|200px]]
  
 
It is the force exerted on a surface by the air above it as gravity pulls it to earth. Atmospheric pressure is commonly measured with a barometer. In a barometer, a column of mercury in a glass tube rises or falls as the weight of the atmospheric changes. Meteorologists describe the atmospheric pressure by how high the mercury rises.
 
It is the force exerted on a surface by the air above it as gravity pulls it to earth. Atmospheric pressure is commonly measured with a barometer. In a barometer, a column of mercury in a glass tube rises or falls as the weight of the atmospheric changes. Meteorologists describe the atmospheric pressure by how high the mercury rises.
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Atmosphere (atm) is a unit of measurement equal to the average air pressure at sea level at a temperature of 15 degrees Celsius (59 degrees Fahrenheit). One atmosphere is 1.013 milibars, or 760 millimeters (29.92 inches) of mercury.
 
Atmosphere (atm) is a unit of measurement equal to the average air pressure at sea level at a temperature of 15 degrees Celsius (59 degrees Fahrenheit). One atmosphere is 1.013 milibars, or 760 millimeters (29.92 inches) of mercury.
  
Atmospheric pressure drops as altitude increases. The atmospheric pressure on Denali, Alaska, is about half that of Honolulu, Hawai'i. Honolulu is a city at sea level. Denali, also known as Mount McKinley, is the highest peak in North America.
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'''Atmospheric pressure''' is also called the '''barometric pressure''' and varies with elevation above sea level. Also, at a given place it varies slightly from time to time because of changes in meteorological conditions.
As the pressure decreases, the amount of oxygen available to breathe also decreases. At very high altitudes, atmospheric pressure and available oxygen get so low that people can become sick and even die.
 
 
 
Mountain climbers use bottled oxygen when they ascend very high peaks. They also take time to get used to the altitude because quickly moving from higher pressure to lower pressure can cause decompression sickness. Decompression sickness, also called "the bends", is also a problem for scuba divers who come to the surface too quickly.
 
  
Aircraft create artificial pressure in the cabin so passengers remain comfortable while flying.
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In siphonic system, local atmospheric pressure (which depends on elevation above sea level and meteorological conditions) is used to determine the allowable negative pressure. Standard atmospheric pressure at sea level and 15°C is equivalent to a value of H_"o"  of about 10.3 m water head.
  
Atmospheric pressure is an indicator of weather. When a low-pressure system moves into an area, it usually leads to cloudiness, wind, and precipitation. High-pressure systems usually lead to fair, calm weather.
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The negative pressure below which cavitation can occur in the pipework of a siphonic system depends on the velocity of the flow, the degree of turbulence in the flow, the value of atmospheric pressure, and the vapour pressure at the relevant temperature of the rainwater.
  
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Where the pipe material is known to be susceptible to damage by cavitation, the minimum design value of pressure head in the pipework should not be lower than (2.5- H_"o" )m; otherwise the minimum pressure should be not lower than (1.5- H_"o" )m, provided in all cases that the corresponding flow velocity at the point of minimum pressure is not greater than 6 m/s. If the velocity 6 m/s, a less negative value of minimum pressure head is necessary in order to prevent possible cavitation problems.
  
 
== References ==
 
== References ==
1. http://www.nationalgeographic.org/encyclopedia/atmospheric-pressure/
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# http://www.nationalgeographic.org/encyclopedia/atmospheric-pressure/
 
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# Fluid Mechanics with Engineering Applications by Robert L. Daugherty, Joseph B. Franzini, E. John Finnemore (p.29)
2. Fluid Mechanics with Engineering Applications (p.29)
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# http://www.srh.noaa.gov/jetstream/atmos/pressure.html
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# http://www.as.wvu.edu/~rbrundage/chapter13a/sld011.html

Latest revision as of 11:24, 21 March 2017

Atmospheric pressure mb heights.jpg
Atmospheric Pressure.jpeg

It is the force exerted on a surface by the air above it as gravity pulls it to earth. Atmospheric pressure is commonly measured with a barometer. In a barometer, a column of mercury in a glass tube rises or falls as the weight of the atmospheric changes. Meteorologists describe the atmospheric pressure by how high the mercury rises.

Atmosphere (atm) is a unit of measurement equal to the average air pressure at sea level at a temperature of 15 degrees Celsius (59 degrees Fahrenheit). One atmosphere is 1.013 milibars, or 760 millimeters (29.92 inches) of mercury.

Atmospheric pressure is also called the barometric pressure and varies with elevation above sea level. Also, at a given place it varies slightly from time to time because of changes in meteorological conditions.

In siphonic system, local atmospheric pressure (which depends on elevation above sea level and meteorological conditions) is used to determine the allowable negative pressure. Standard atmospheric pressure at sea level and 15°C is equivalent to a value of H_"o" of about 10.3 m water head.

The negative pressure below which cavitation can occur in the pipework of a siphonic system depends on the velocity of the flow, the degree of turbulence in the flow, the value of atmospheric pressure, and the vapour pressure at the relevant temperature of the rainwater.

Where the pipe material is known to be susceptible to damage by cavitation, the minimum design value of pressure head in the pipework should not be lower than (2.5- H_"o" )m; otherwise the minimum pressure should be not lower than (1.5- H_"o" )m, provided in all cases that the corresponding flow velocity at the point of minimum pressure is not greater than 6 m/s. If the velocity 6 m/s, a less negative value of minimum pressure head is necessary in order to prevent possible cavitation problems.

References

  1. http://www.nationalgeographic.org/encyclopedia/atmospheric-pressure/
  2. Fluid Mechanics with Engineering Applications by Robert L. Daugherty, Joseph B. Franzini, E. John Finnemore (p.29)
  3. http://www.srh.noaa.gov/jetstream/atmos/pressure.html
  4. http://www.as.wvu.edu/~rbrundage/chapter13a/sld011.html