Page:1|2|3|4|5|6|7|8|9|10
   
 
Spring 2001 Update

Accurate bearing determination can best be accomplished by using only the cloud-ground return stroke signals, and so we need a reliable method for rejecting the intracloud signals. Intracloud strokes lead to phase distortions and ambiguous bearings at a remote receiver because their radiated fields have frequent horizontal components and so are propagated along multiple paths of ionospheric reflections (sky wave) and surface waves. In contrast, vertical return strokes, whose propagation is largely confined to surface waves, are propagated along this shortest single path. Use of the broadband, gated technique along with software analysis accomplishes the required discrimination. Fortunately the wave forms of intracloud strokes are usually quite distinct from those produced by return strokes. The intracloud wave form is usually biphasic (some prefer the term bipolar) showing a very large overshoot (E2) of reversed polarity following the initial excursion (E1). In contrast, return strokes tend to be monophasic (or monopolar), in that there is a relatively small overshoot following the initial wave component. These rather distinct signatures allow software sorting of the two stroke types and selection of only the return stroke for locating purposes.
 

 
A pair of voltage field wave forms from intracloud strokes recorded at Lawrence, Kansas on September 28, 1995 from a thunderstorm about 200 km away. Note the distinctly biphasic shape and relative magnitudes of the two peaks E1 and E2.
 
 
A voltage field wave form from a negative return stroke recorded on the same date as that for the above intracloud stroke. Note that there is no pronounced overshoot E2 and that the wave shape is basically monophasic. The additional rises in the voltage field following the peak E1 are characteristic of the first return stroke in a flash.
 
Note: If a search engine brought you directly to this page, then go to the GP-1 Start Page.
The Web address for the GP-1 Start Page is http://bub2.met.psu.edu/default.htm

Page 4 of 10
Page:1|2|3|4|5|6|7|8|9|10