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Home > History and Archaeology > History > The Structure of the Atmosphere in Clear Weather; A Study of Soundings with Pilot Balloons
The Structure of the Atmosphere in Clear Weather; A Study of Soundings with Pilot Balloons

The Structure of the Atmosphere in Clear Weather; A Study of Soundings with Pilot Balloons


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About the Book

This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1912 Excerpt: ... Fig. 37. Feb. 2nd, 1908, C p.m. a. Surface isobars, b. Computed isobars at 3 kilometres, showing relative differences of pressure from that over Portland Bill. Fig. 38. Diagram showing gradient and surface wind directions in Class (c). Decreasing velocity. the upper layers the depression is a southward extension of the polar low pressure system; the slackening of the wind velocity in the upper layers on the polar side of a cyclone quite corroborates this view. With regard to the wind direction in this class it has been pointed out above that the surface wind is nearly always backed with regard to the gradient wind. In some cases the gradient direction is never reached; but it is reached or the nearest approach to it is reached a little above the point of maximum velocity. At higher levels there is sometimes a backing towards a Northerly or North-Easterly point, and sometimes the wind remains Easterly up to the highest point reached. In a few cases there is considerable veering in the upper layers; for instance on May 16th, 1909. Examples of an Easterly wind being found at great heights occur on May 6th and 7th, 1909, on Aug. 5th, 1909, and on March 3rd, 1910. On May 6th and 7th, 1909, the direction remained from East to South-East up to the level of the Stratosphere; on Aug. 5th, 1909, it remained between North and East up to 8 kilometres, when there was a discontinuity, the wind above being South-East up to 12 kilometres, when all real wind seems to have ceased. On March 3rd, 1910, the wind after being South-East at 3 kilometres slowly backed to North at 8 kilometres and remained between North and North-East to 11 kilometres when the peculiar wind conditions of the stratosphere were reached. Class (d). Reversals or great changes of direction in the Upper ...


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Product Details
  • ISBN-13: 9781231235928
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 32
  • Spine Width: 2 mm
  • Width: 189 mm
  • ISBN-10: 1231235926
  • Publisher Date: 01 May 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 77 gr

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