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pubmed-article:17819546rdf:typepubmed:Citationlld:pubmed
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pubmed-article:17819546pubmed:dateCreated2010-6-8lld:pubmed
pubmed-article:17819546pubmed:abstractTextMeasurements of the magnetic field and earth current in the vicinity of a tornado show large steplike deflections coincident with the touching down of the funnel. Calculations with a simple current model indicate that a minimum current of several hundred amperes must be postulated to account for the observed deflection in magnetic field. The existence of a steady current of 225 amperes for a period of about 10 minutes provides joule heat at the rate of approximately 10(10) joules per second, and involves a total charge transfer of 135,000 coulombs. The calculations imply that a tornado is electrically equivalent to several hundred isolated thunderstorm cells active simultaneously.lld:pubmed
pubmed-article:17819546pubmed:languageenglld:pubmed
pubmed-article:17819546pubmed:journalhttp://linkedlifedata.com/r...lld:pubmed
pubmed-article:17819546pubmed:statusPubMed-not-MEDLINElld:pubmed
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pubmed-article:17819546pubmed:issn0036-8075lld:pubmed
pubmed-article:17819546pubmed:authorpubmed-author:BrookMMlld:pubmed
pubmed-article:17819546pubmed:issnTypePrintlld:pubmed
pubmed-article:17819546pubmed:day22lld:pubmed
pubmed-article:17819546pubmed:volume157lld:pubmed
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pubmed-article:17819546pubmed:pagination1434-6lld:pubmed
pubmed-article:17819546pubmed:year1967lld:pubmed
pubmed-article:17819546pubmed:articleTitleElectric currents accompanying tornado activity.lld:pubmed
pubmed-article:17819546pubmed:publicationTypeJournal Articlelld:pubmed