Difference between revisions of "AY Honors/Weather - Advanced/Answer Key"

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[[Image:IntertropicalConvergenceZone-EO.jpg|right|300px|thumb|The thunderstorms of the Intertropical Convergence Zone form a line across the eastern Pacific Ocean.]]
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[[Image:Max Min Thermometer.JPG|250px|right|thumb|A Maximum Minimum thermometer, also known as Six’s thermometer after its inventor. The scales are Fahrenheit on the inside of the U and Centigrade on the outside. The current temperature is 23 Centigrade, The maximum recorded is 25, and the minimum is 15, both read from the base of the small markers in each arm of the U tube. The bulbs are hidden by a plastic housing]]
  
The '''Intertropical convergence zone''' '''(ITCZ)''', also known as the '''Intertropical Front''' or the '''Equatorial Convergence Zone''', is a belt of [[low pressure area|low pressure]] girdling [[Earth]] at the [[equator]]. It is formed, as its name indicates, by the [[convergence]] of warm, moist air from the latitudes above and below the equator.
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'''Six's thermometer''' is a [[thermometer]] which can measure the [[maximum]] and [[minimum]] [[temperature]] during a given time, devised by [[James Six]] in [[1782]]. It is also known as a '''Maximum minimum thermometer'''. It is still in common use wherever a simple way is needed to measure the extremes of temperature at a location, e.g. in [[meteorology]] and [[horticulture]].
  
The air is drawn in to the intertropical convergence zone by the action of the [[Hadley cell]], a [[scale (spatial)|macroscale]] [[earth's atmosphere|atmospheric]] feature which is part of the Earth's heat and moisture distribution system. It is transported aloft by the [[convection|convective]] activity of [[thunderstorm]]s; regions in the intertropical convergence zone receive [[precipitation (meteorology)|precipitation]] more than 200 days in a year.
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==Description==
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It consists of a U-shaped capillary tube with two separate temperature readings, one for the maximum temperature and one for the minimum temperature. There are bulbs at the top of each arm of the U-shaped tube. The one at the top of the minimum reading scale contains [[alcohol]], the other contains a [[vacuum]] or low pressure alcohol vapour.  
  
The location of the intertropical convergence zone varies over time, as it moves back and forth across the equator in a semiannual pattern, following the sun's [[zenith]] point. There is also a [[diel|diurnal]] cycle, with [[cumulus cloud|cumulus]] developing around midday and building to thunderstorms in mid to late afternoon.
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In the bend of the U is a section of [[mercury (element)|mercury]] which is pushed around the tube by the expansion and contraction of the alcohol in the first bulb. It is the alcohol which measures the temperature, the mercury indicates the temperature reading on both scales. At any given time the position of the mercury should be the same on both the maximum and minimum scales. If not then the instrument scales are not correctly positioned.
  
Variation in the location of the intertropical convergence zone drastically affects rainfall in many equatorial [[nation]]s, resulting in the wet and dry seasons of the tropics rather than the cold and warm seasons of higher latitudes. Longer term changes in the intertropical convergence zone can result in severe droughts or flooding in nearby areas.
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As the mercury moves it pushes 2 small steel markers which are sprung into the tube. They record the furthest point reached by the mercury in each arm of the tube. When the temperature reverses and the mercury is moved in the opposite direction by the expansion or contraction of the alcohol, the sprung markers remain in the tube at the furthest position they have been pushed by the mercury. They thus record the extremes of temperature experienced by the devise since it was last reset.
  
Because of the strength of the Hadley cells on either side of it, weather systems familiar to mid-latitude dwellers do not have the chance to form, and as a result, there are no [[prevailing winds]]. Advective (horizontal) motion is due entirely to air from the [[trade winds]] replacing that carried aloft by [[convection]], a slow, languorous process at best.  
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The markers are reset by using a small [[magnet]] which can drag the markers along the tube so that they again rest on the surface of the mercury. In some designs the tube is [[horizontal]] and the markers un-sprung so the devise is reset by turning it to the [[vertical]] so that [[gravity]] returns the markers to the mercury.
  
Early sailors named this belt of calm '''the doldrums''' because of the low spirits they found themselves in after days of no wind. To find oneself becalmed in this region in a hot and muggy climate could mean death in the era when wind was the only motive force.
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Its important to note that the alcohol is used as the thermometric liquid, which batty boys also drink sometimes to get very drunk and, and as a side-effect of getting drunk, you could wake up in a bin. so beware.
  
ŵ==References==
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==References==
*[http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=4028 Short NASA article with high resolution photo]
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*''A History of the Thermometer and Its Uses in Meteorology'' by W. E. Knowles Middleton, Johns Hopkins University Press, 1966; ISBN 0801871530
  
[[Category:Tropical cyclone meteorology]]
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*''The Construction of a Thermometer'' by James Six, Nimbus Publishing Ltd,1980; ISBN: 0950703605
  
[[de:Innertropische Konvergenzzone]]
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==External links==
[[es:Zona de convergencia intertropical]]
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*[http://brunelleschi.imss.fi.it/genscheda.asp?appl=SIM&xsl=catalogo&indice=54&lingua=ENG&chiave=410041 Article on Six thermometer at the Museum of the History of Science at Florence , Italy]
[[fr:Zone de convergence intertropicale]]
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[[nl:Doldrum]]
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[[no:Den intertropiske konvergenssonen]]
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*[http://www.syvum.com/cgi/online/serve.cgi/squizzes/physics/thermometers.html Explanation of the working of Six's thermometer]
[[nn:Den intertropiske konvergenssonen]]
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[[sv:Intertropiska konvermbgenszonen]]
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[[Category:Thermometers]]

Revision as of 16:57, 23 March 2006

A Maximum Minimum thermometer, also known as Six’s thermometer after its inventor. The scales are Fahrenheit on the inside of the U and Centigrade on the outside. The current temperature is 23 Centigrade, The maximum recorded is 25, and the minimum is 15, both read from the base of the small markers in each arm of the U tube. The bulbs are hidden by a plastic housing

Six's thermometer is a thermometer which can measure the maximum and minimum temperature during a given time, devised by James Six in 1782. It is also known as a Maximum minimum thermometer. It is still in common use wherever a simple way is needed to measure the extremes of temperature at a location, e.g. in meteorology and horticulture.

Description

It consists of a U-shaped capillary tube with two separate temperature readings, one for the maximum temperature and one for the minimum temperature. There are bulbs at the top of each arm of the U-shaped tube. The one at the top of the minimum reading scale contains alcohol, the other contains a vacuum or low pressure alcohol vapour.

In the bend of the U is a section of mercury which is pushed around the tube by the expansion and contraction of the alcohol in the first bulb. It is the alcohol which measures the temperature, the mercury indicates the temperature reading on both scales. At any given time the position of the mercury should be the same on both the maximum and minimum scales. If not then the instrument scales are not correctly positioned.

As the mercury moves it pushes 2 small steel markers which are sprung into the tube. They record the furthest point reached by the mercury in each arm of the tube. When the temperature reverses and the mercury is moved in the opposite direction by the expansion or contraction of the alcohol, the sprung markers remain in the tube at the furthest position they have been pushed by the mercury. They thus record the extremes of temperature experienced by the devise since it was last reset.

The markers are reset by using a small magnet which can drag the markers along the tube so that they again rest on the surface of the mercury. In some designs the tube is horizontal and the markers un-sprung so the devise is reset by turning it to the vertical so that gravity returns the markers to the mercury.

Its important to note that the alcohol is used as the thermometric liquid, which batty boys also drink sometimes to get very drunk and, and as a side-effect of getting drunk, you could wake up in a bin. so beware.

References

  • A History of the Thermometer and Its Uses in Meteorology by W. E. Knowles Middleton, Johns Hopkins University Press, 1966; ISBN 0801871530
  • The Construction of a Thermometer by James Six, Nimbus Publishing Ltd,1980; ISBN: 0950703605

External links