A numerical study of the effect of cloud nuclei on the initiation of rain from warm clouds

dc.contributor.authorLee, Seung-Man
dc.date.accessioned2009-07-15T18:00:06Z
dc.date.available2009-07-15T18:00:06Z
dc.date.issued1978
dc.descriptionTypescript.
dc.descriptionTheses (Ph. D.)--University of Hawaii at Manoa, 1978.
dc.descriptionBibliography: leaves 85-89.
dc.descriptionMicrofiche.
dc.descriptionviii, 89 leaves ill
dc.description.abstractThe effects of the cloud nucleus size distribution and number concentration on rain initiation from shallow maritime warm clouds are examined in a one-dimensional, time-dependent cylindrical cloud model. Calculations include nucleation, condensation on both nuclei and drops, collection of drops and scavenging of nucleus-size particles to drops. It was found that nuclei of mass about 10^-15 g are most efficient for warm rain development and the number concentration normally observed near Hawaii is the optimum concentration for maximum rainfall.
dc.identifier.urihttp://hdl.handle.net/10125/9972
dc.language.isoen-US
dc.relationTheses for the degree of Doctor of Philosophy (University of Hawaii at Manoa). Meteorology; no. 1106
dc.rightsAll UHM dissertations and theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission from the copyright owner.
dc.subjectCloud physics -- Mathematical models
dc.subjectCondensation (Meteorology)
dc.titleA numerical study of the effect of cloud nuclei on the initiation of rain from warm clouds
dc.typeThesis
dc.type.dcmiText

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