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Electrical phenomena of falling and drifting snow

dc.contributor.advisorCurrie, B. W.en_US
dc.creatorPearce, Douglas Campbellen_US
dc.date.accessioned2010-08-11T10:39:35Zen_US
dc.date.accessioned2013-01-04T04:52:26Z
dc.date.available2011-08-11T08:00:00Zen_US
dc.date.available2013-01-04T04:52:26Z
dc.date.created1948en_US
dc.date.issued1948en_US
dc.date.submitted1948en_US
dc.description.abstractSince the time of Franklin, 1750, it has been known that there is a state of electricity associated with the Earth and its atmosphere. Experiments have shown that a total negative surface charge of the order of 5 x 105 coulombs resides on the Earth. This gives rise to the Earth's normal fair-weather electric field of an average magnitude of approximately 100 volts per meter. Furthermore, the atmosphere has a finite conductivity, so that under the action of this electric field, there is a dissipation current. … Observations from balloon ascents (Wigand, 1) have shown that the Earth's electric field decreases far more rapidly with altitude than that due to a uniform distribution of charge on the surface. This indicates the existence of a free space charge. The distribution of this free space charge determines uniquely, through Poisson's equation, the electrical state of the atmosphere. Thus, a study of this charge distribution is extremely important. Free charges result from conduction in the non-homogeneous atmosphere, and from accelerating forces acting on rain, snow and dust.en_US
dc.identifier.urihttp://hdl.handle.net/10388/etd-08112010-103935en_US
dc.language.isoen_USen_US
dc.titleElectrical phenomena of falling and drifting snowen_US
dc.type.genreThesisen_US
dc.type.materialtexten_US
thesis.degree.departmentPhysicsen_US
thesis.degree.disciplinePhysicsen_US
thesis.degree.grantorUniversity of Saskatchewanen_US
thesis.degree.levelMastersen_US
thesis.degree.nameMaster of Science (M.Sc.)en_US

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