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Southern oscillation and its effect on tornadic activity in the United States

dc.contributor.authorKnowles, John B., author
dc.contributor.authorPielke, Roger A., Sr., author
dc.date.accessioned2022-03-04T15:52:10Z
dc.date.available2022-03-04T15:52:10Z
dc.date.issued2005-03-31
dc.descriptionPublished as an Atmospheric Science Paper March 31, 2005 and November 5, 1993 on title page.
dc.description.abstractThe Southern Oscillation has been shown in previous research to cause changes in the weather patterns over the continental United States. These changes, caused by either the warm El Nino or cold La Nina, could potentially effect numbers, locations, and strengths of tornadoes in the United States. Using a variation of the Southern Oscillation Index, the seven strongest El Nino and five strongest La Nina events during the period 1953-1989 were examined to see what effect, if any, that they would have on: 1) Total tornado numbers, 2) Violent tornado track length, 3) Violent tornado numbers, and 4) ?:40 tornado outbreaks. Little difference was found in total tornado numbers between El Nino and La Nina events. However, significant differences were found in the number of violent tornadoes, and in large number tornado outbreaks. La Nina event years were found to have longer than average track lengths, more violent tornadoes, and a good probability of having an outbreak of 40 or more tornadoes. El Nino event years were found to have shorter than average track lengths, less violent tornadoes, and only a slim possibility of having an outbreak. Possible reasons for the above conclusions include: 1) Warmer than normal temperatures in the western U.S./Canada along with cooler than normal temperatures in the southern U.S. during El Nino years; and 2) Colder than normal temperatures in the west­ ern U.S./Canada along with warmer than normal temperatures in the southern U.S. during La Nina years. This would act to weaken/strengthen the interactions between warm and cold air in the midwest U.S. during El Nino/La Nina event years and decrease/increase the numbers and lengths of violent tornadoes.
dc.description.sponsorshipSponsored by the National Science Foundation grant number ATM-9017849.
dc.format.mediumreports
dc.identifier.urihttps://hdl.handle.net/10217/234507
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relationCatalog record number (MMS ID): 991021250089703361
dc.relationQC852 .C6 no. 755
dc.relation.ispartofAtmospheric Science Papers (Blue Books)
dc.relation.ispartofAtmospheric science paper, no. 755
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subjectSouthern oscillation
dc.subjectTornadoes -- United States
dc.titleSouthern oscillation and its effect on tornadic activity in the United States
dc.typeText
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