{"id":{"repo_id":"uiuc","oai_identifier":"oai:www.ideals.illinois.edu:2142/85973"},"canonical_url":"https://search.dev.ndltd.org/etd/uiuc/oai:www.ideals.illinois.edu:2142/85973","repository":{"repo_id":"uiuc","name":"University of Illinois - Urbana-Champaign","base_url":"https://www.ideals.illinois.edu/oai-pmh"},"display":{"title":"The Development, Evolution, and Forcing of the Rear Inflow Jet in Bow Echoes During BAMEX","abstract":"Simulations revealed that observations of a sharp change in the RH profile across the melting layer, from saturated air with respect to ice above to subsaturated air with respect to water below, can develop in response to microphysical processes alone. However, dynamic processes, such as sufficiently strong downdrafts, may allow the air to remain subsaturated for T < 0&deg;C. Sensitivity tests revealed that in the absence of dynamic processes, the dichotomy in the RH field across the melting level always developed.","abstract_html":"Simulations revealed that observations of a sharp change in the RH profile across the melting layer, from saturated air with respect to ice above to subsaturated air with respect to water below, can develop in response to microphysical processes alone. However, dynamic processes, such as sufficiently strong downdrafts, may allow the air to remain subsaturated for T &lt; 0&amp;deg;C. Sensitivity tests revealed that in the absence of dynamic processes, the dichotomy in the RH field across the melting level always developed.","abstract_has_math":false,"creators":["Grim, Joseph A."],"institution":"University of Illinois at Urbana-Champaign","degree_name":"Ph.D.","degree_level":"Dissertation","degree_discipline":"Atmospheric Sciences","degree_department":null,"school":null,"contributors":["Robert Rauber"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2015,"date_issued":"2015-09-28T14:52:23Z","date_published":"2015-09-28T14:52:23Z","updated_at":"2026-07-22T22:26:26Z","subjects":["Remote Sensing"],"languages":["eng"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["(MiAaPQ)AAI3301140"],"render_values":[{"text":"(MiAaPQ)AAI3301140","href":null,"code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/2142/85973","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Robert Rauber"]},{"key":"dc:creator","label":"Author","values":["Grim, Joseph A."]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["2015-09-28T14:52:23Z","10000-01-01","2007"]},{"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":["Remote Sensing"]}]},{"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/2142/85973","(MiAaPQ)AAI3301140"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["Simulations revealed that observations of a sharp change in the RH profile across the melting layer, from saturated air with respect to ice above to subsaturated air with respect to water below, can develop in response to microphysical processes alone. 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