|
![]() ![]() Vydáno dne 26. 12. 2013 (140 přečtení) v angličtině (mimochodem já tvrdím něco podobnýho a nezávisle na tomto textu od roku 2006 a loni jsem o tom psal taky - ovšem u nás bez odezvy) it? In 1925, C. T. R. Wilson proposed a mechanism by which electrical discharge from lightning storms could propagate upwards from clouds to the ionosphere. Around the same time, Robert Watson-Watt, working at the Radio Research Station in Slough, UK, suggested that the ionospheric sporadic E layer (Es) appeared to be enhanced as a result of lightning but that more work was needed. In 2005, C. Davis and C. Johnson, working at the Rutherford Appleton Laboratory in Oxfordshire, UK, demonstrated that the Es layer was indeed enhanced as a result of lightning activity. Their subsequent research has focussed on the mechanism by which this process can occur. http://en.wikipedia.org/wiki/Ionosphere#Lightning Jurgen Bartels Suellwarden, N. Germany -------------------- http://krysatec.benghi.org/phprs/view.php?cisloclanku=2012060902 A následně psal Jurgen tohle:
formation. But they did not rule out that it exists, only their result did not prove it. More research is required. Many DXer (myself included) have observed Es signals right before a local T-storm approached but not when it had passed thru. That speaks against all theories of refraction at path midway, and might just be pure coincidence. ( Celý článek | Autor: administrator | Počet komentářů: 0 | Přidat komentář | ![]() ![]() |
|
Powered by phpRS. Sponsored by benghi.org