{"id":{"repo_id":"uiuc","oai_identifier":"oai:www.ideals.illinois.edu:2142/85956"},"canonical_url":"https://search.dev.ndltd.org/etd/uiuc/oai:www.ideals.illinois.edu:2142/85956","repository":{"repo_id":"uiuc","name":"University of Illinois - Urbana-Champaign","base_url":"https://www.ideals.illinois.edu/oai-pmh"},"display":{"title":"The Structure and Intensity of Winter Mesoscale Lake -Effect Circulations Associated With an Isolated Lake","abstract":"To understand and predict the strength of mesoscale lake-effect circulations a simple function, called the lake-effect intensity index, was developed using the dimensional analysis technique. The intensity index was found to be equivalent to scaling the Froude number by a dimensionless quantity comprised of lake-air temperature difference, fetch distance, air temperature, and boundary layer height to improve its predictive capability. The intensity index: (1) accounts for the relative contributions of variables fundamental to the lake-effect system, (2) effectively predicts the strength of lake-effect circulations from first order fundamental variables that are easily measured, and (3) can be used regardless of the lake-effect morphological regime.","abstract_html":"To understand and predict the strength of mesoscale lake-effect circulations a simple function, called the lake-effect intensity index, was developed using the dimensional analysis technique. The intensity index was found to be equivalent to scaling the Froude number by a dimensionless quantity comprised of lake-air temperature difference, fetch distance, air temperature, and boundary layer height to improve its predictive capability. The intensity index: (1) accounts for the relative contributions of variables fundamental to the lake-effect system, (2) effectively predicts the strength of lake-effect circulations from first order fundamental variables that are easily measured, and (3) can be used regardless of the lake-effect morphological regime.","abstract_has_math":false,"creators":["Laird, Neil Francis"],"institution":"University of Illinois at Urbana-Champaign","degree_name":"Ph.D.","degree_level":"Dissertation","degree_discipline":"Atmospheric Sciences","degree_department":null,"school":null,"contributors":["David Kristovich"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2015,"date_issued":"2015-09-28T14:52:17Z","date_published":"2015-09-28T14:52:17Z","updated_at":"2026-07-22T22:26:26Z","subjects":["Geophysics"],"languages":["eng"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["(MiAaPQ)AAI3023107"],"render_values":[{"text":"(MiAaPQ)AAI3023107","href":null,"code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/2142/85956","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["David Kristovich"]},{"key":"dc:creator","label":"Author","values":["Laird, Neil Francis"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["2015-09-28T14:52:17Z","10000-01-01","2001"]},{"key":"dc:type","label":"Dc Type","values":["text"]},{"key":"thesis:degree_discipline","label":"Discipline","values":["Atmospheric Sciences"]},{"key":"thesis:degree_level","label":"Degree Level","values":["Dissertation"]},{"key":"thesis:degree_name","label":"Degree Name","values":["Ph.D."]},{"key":"thesis:institution_name","label":"Thesis Institution Name","values":["University of Illinois at Urbana-Champaign"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Geophysics"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language","label":"Dc Language","values":["eng"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["http://hdl.handle.net/2142/85956","(MiAaPQ)AAI3023107"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["To understand and predict the strength of mesoscale lake-effect circulations a simple function, called the lake-effect intensity index, was developed using the dimensional analysis technique. 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The intensity index was found to be equivalent to scaling the Froude number by a dimensionless quantity comprised of lake-air temperature difference, fetch distance, air temperature, and boundary layer height to improve its predictive capability. The intensity index: (1) accounts for the relative contributions of variables fundamental to the lake-effect system, (2) effectively predicts the strength of lake-effect circulations from first order fundamental variables that are easily measured, and (3) can be used regardless of the lake-effect morphological regime.","Made available in DSpace on 2015-09-28T14:52:17Z (GMT). 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