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Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/4114
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dc.contributor.authorVenkatakrishnan, P-
dc.date.accessioned2008-12-18T14:18:39Z-
dc.date.available2008-12-18T14:18:39Z-
dc.date.issued1982-11-
dc.identifier.citationSolar Physics, Vol. 81, pp. 193 - 195.en
dc.identifier.issn0038-0938-
dc.identifier.urihttp://hdl.handle.net/2248/4114-
dc.descriptionOpen Access-
dc.description.abstractThe observed effects of solar flares and interplanetary sector crossings seem to indicate that particle precipitation in the earth's upper atmosphere decreases cyclonic activity in the troposphere. As an extrapolation to longer term effects, it is suggested that the recurrence of prolonged periods of enhanced solar wind particle precipitation in the upper atmosphere during alternate solar minima could cause the recurrence of extreme droughts.en
dc.language.isoenen
dc.publisherD. Reidel Publishing Coen
dc.relation.urihttp://adsabs.harvard.edu/abs/1982SoPh...81..193Ven
dc.relation.urihttp://www.springerlink.com/content/x5512041336157r6/en
dc.rights© D. Reidel Publishing Coen
dc.subjectAtmospheric Circulationen
dc.subjectDroughten
dc.subjectParticle Precipitationen
dc.subjectSolar Activity Effectsen
dc.subjectSolar Terrestrial Interactionsen
dc.subjectSolar Winden
dc.subjectAnticyclonesen
dc.subjectInterplanetary Magnetic Fieldsen
dc.subjectSolar Flaresen
dc.subjectTropospheric Wavesen
dc.titleInfluence of solar wind variability of the recurrence of droughtsen
dc.typeArticleen
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