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Weather Forecasting in the United States

Weather Forecasting in the United States


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Purchase of this book includes free trial access to www.million-books.com where you can read more than a million books for free. This is an OCR edition with typos. Excerpt from book: pressure gradient the tangential component of the force will then check the motion. Such a condition signifies that the actual velocity is already greater than the gradient velocity. The forces are graphically indicated for certain representative cases in figure 1. From the foregoing simple considerations it appears that the forces governing the motions of relatively free-air masses in a cyclonic system tend automatically to establish and maintain a condition of equilibrium in which the velocity of motion is practically the gradient velocity, and the direction of motion then becomes parallel with the isobars. Fio. 1.?Boheme to depict forces cautiny and modifutny .(nrf4.?Pressure gradient In lndicated by short arrows crossing line of motion near the middle. Heavy body portion of line indicates component of gradient tending to overcome resistance, or increase or retard velocity. A and / are deflective forces due to earth and gradient, respectively. Heavy portion of one of these forces is dominating component, and remainder of same force equals and neutralizes the force on the opposite side. Centrifugal forces, in the ordinary meaning of the word, have no existence in any of the instances Illustrated. Sometimes /i sometimes f2 acts from the center outwardly. These may then properly be called centrifugal forces, but they are entirely different in origin and magnitude from the inertia reaction commonly designated centrifugal force. Although equation (G) applies strictly only to certain ideal conditions, nevertheless it must be recognized that other cases are also represented, in which the force f.2 comprises, not the whole pressure gradient effect, but only a component thereof. The velocity will then not be the true gradient velocity and the wind direction will cross the isob...


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Product Details
  • ISBN-13: 9780217419390
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 140
  • Spine Width: 8 mm
  • Width: 189 mm
  • ISBN-10: 0217419399
  • Publisher Date: 15 May 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 263 gr


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