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  • Irish Chronicles Document Links Between Volcanoes and Weather
    A study of over 40,000 written entries in Irish Annals and ice core measurements shows a strong corr...Read more

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    Irish Chronicles Document Links Between Volcanoes and Weather

    A study of over 40,000 written entries in Irish Annals and ice core measurements shows a strong correlation between the occurrence of volcanic eruptions and extreme cold weather in Ireland over a 1200 year period. Data analyzed in this study cover the period from 431 to 1649, during which time up to 48 volcanic eruptions are identified in Greenland ice core records through deposition of volcanic sulfate in annual layers of ice. You can find the study (open access), published on 6 June 2013 in IOP Publishing's journal Environmental Research Letters, at http://iopscience.iop.org/1748-9326/8/2/024035/article. Find out more about how volcanoes can influence climate.
  • EF-5 Tornado in El Reno, Oklahoma Widest Ever Recorded in US
    The EF-5 tornado that hit El Reno, Oklahoma on May 31st was the widest ever recorded in the US, acco...Read more

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    EF-5 Tornado in El Reno, Oklahoma Widest Ever Recorded in US

    The EF-5 tornado that hit El Reno, Oklahoma on May 31st was the widest ever recorded in the US, according to the National Weather Service in Norman Oklahoma. The tornado, which remained on the ground for 40 minutes and reached 2.6 miles across (4.2 km), took the lives of 18 people including storm chasers Tim Samaras, Paul Samaras and Carl Young. For more information on the tornado, visit http://ow.ly/i/2hfDG.
  • Atmospheric CO2 Level Tops 400 ppm
    During the week of May 13th, the CO2 level at the Mauna Loa Observatory in Hawaii topped 400 ppm rep...Read more

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    Atmospheric CO2 Level Tops 400 ppm

    During the week of May 13th, the CO2 level at the Mauna Loa Observatory in Hawaii topped 400 ppm repeatedly. Daily levels of CO2 can vary due to weather, and there are seasonal trends as well. The level of atmospheric greenhouse gases continues to increase, now over 120 ppm since the Industrial Revolution began. For more on the Keeling Curve, see http://keelingcurve.ucsd.edu/. Find out more about greenhouse gases and warming.

Why is it that the air traveling over the top of the airfoil has to reach the end of it at the same time that the air traveling underneath the airfoil reaches it.

The idea that the air traveling over the top of the airfoil must reach the end of the wing at the same time as the air traveling along the bottom of the airfoil is called the 'principle of equal transit times.' This follows from Bernoulli's principle, which says that when fluid velocity increases, pressure decreases. As the air over the top of the airfoil has higher velocity than that of air at the bottom of the airfoil, there is a decrease in pressure at the top of the airfoil, which causes lift. This explanation of lift is actually inaccurate. The reason this explanation has been around for so long is that it is the easiest to understand.

The Bernoulli principle is true, as is the fact that the air at the top of the airfoil goes faster than that at the bottom. However, it is untrue that the seperated air must reach the end of the airfoil at the same time. In reality, the air at the bottom of the airfoil is slowed down.

In order to reach the correct explanation, we need to look at Newton's laws. The third law says that for every action there is an equal and opposite reaction. In order for an airfoil to produce lift, it must obtain an equal and opposite reaction. So, an airfoil changes the direction of the air: it sends a stream of air downward, in order to send the wing upward. (See picture.) The lift of an airfoil is proportional to the amount of air diverted downward times the downward velocity of the air. The more air the airfoil sends downward (by changing the shape or angle of the airfoil), the more lift will be obtained. For a more detailed description, and more information on flight, you might try the ALLSTAR Network.


Submitted by Bob (age 20, Maryland, USA)
(August 2, 1999)



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