{"id":{"repo_id":"uiuc","oai_identifier":"oai:www.ideals.illinois.edu:2142/125636"},"canonical_url":"https://search.dev.ndltd.org/etd/uiuc/oai:www.ideals.illinois.edu:2142/125636","repository":{"repo_id":"uiuc","name":"University of Illinois - Urbana-Champaign","base_url":"https://www.ideals.illinois.edu/oai-pmh"},"display":{"title":"A large-scale investigation of soil moisture feedbacks on precipitation intensity in the central United States","abstract":"Submission original under an indefinite embargo labeled 'Open Access'. The submission was exported from vireo on 2025-02-04 without embargo terms","abstract_html":"Submission original under an indefinite embargo labeled &#x27;Open Access&#x27;. The submission was exported from vireo on 2025-02-04 without embargo terms","abstract_has_math":false,"creators":["Lazarow, R. Mitchell"],"institution":"University of Illinois at Urbana-Champaign","degree_name":"M.S.","degree_level":"Thesis","degree_discipline":"Atmospheric Sciences","degree_department":null,"school":null,"contributors":["Ford, Trent"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2024,"date_issued":"2024-07-15","date_published":"2024-07-15","updated_at":"2026-07-22T22:25:02Z","subjects":["Soil Moisture","Thunderstorms","Convection","Land-atmosphere Interactions","Surface Flux"],"languages":["en","eng"],"rights":["Copyright 2024 R. Mitchell Lazarow"],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"https://hdl.handle.net/2142/125636","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Ford, Trent"]},{"key":"dc:creator","label":"Author","values":["Lazarow, R. Mitchell"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["2024-07-15","2024-08"]},{"key":"dc:type","label":"Dc Type","values":["text","Thesis"]},{"key":"thesis:degree_discipline","label":"Discipline","values":["Atmospheric Sciences"]},{"key":"thesis:degree_level","label":"Degree Level","values":["Thesis"]},{"key":"thesis:degree_name","label":"Degree Name","values":["M.S."]},{"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":["Soil Moisture","Thunderstorms","Convection","Land-atmosphere Interactions","Surface Flux"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language","label":"Dc Language","values":["en","eng"]},{"key":"dc:rights","label":"Dc Rights","values":["Copyright 2024 R. Mitchell Lazarow"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["https://hdl.handle.net/2142/125636"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["Submission original under an indefinite embargo labeled 'Open Access'. The submission was exported from vireo on 2025-02-04 without embargo terms","The student, R. Mitchell Lazarow, accepted the attached license on 2024-07-14 at 00:52.","The student, R. Mitchell Lazarow, submitted this Thesis for approval on 2024-07-14 at 00:59.","This Thesis was approved for publication on 2024-07-15 at 15:28.","DSpace SAF Submission Ingestion Package generated from Vireo submission #21113 on 2025-02-04 at 21:05:22","Convective activity, including thunderstorms, significantly influences Earth’s climate and environment while posing substantial risks to society. Understanding the fundamental processes driving these events is crucial, particularly given the projected increase in their occurrence and intensity. Previous studies capture impacts on precipitation occurrence and distribution but lack focus on precipitation intensity, especially at a large scale. Soil moisture affects surface heat fluxes, altering the planetary boundary layer's stability, which influences convective activity. This study examines the relationship between soil moisture and precipitation intensity across the Central United States from 2005 to 2017 using the Thunderstorm Observation by Radar (ThOR) algorithm. The analysis includes over 500,000 thunderstorm data points, correlating soil moisture with storm reflectivity and vertically integrated liquid. Findings indicate a broad negative correlation between soil moisture and precipitation intensity, suggesting that drier soils lead to stronger convective storms. Pathway variables like boundary layer height and evaporative fraction drive the mechanisms by which soil moisture influences storm intensity. The results underscore the importance of soil moisture in modulating convective storm behavior, with implications for improving forecasting and understanding of land-atmosphere interactions. Further research is needed to refine these findings and explore regional variations and other influencing factors."]},{"key":"dc:format","label":"Dc Format","values":["application/pdf"]},{"key":"dc:title","label":"Title","values":["A large-scale investigation of soil moisture feedbacks on precipitation intensity in the central United States"]}]}],"canonical_facts":{"dc:contributor":["Ford, Trent"],"dc:creator":["Lazarow, R. Mitchell"],"dc:date":["2024-07-15","2024-08"],"dc:description":["Submission original under an indefinite embargo labeled 'Open Access'. The submission was exported from vireo on 2025-02-04 without embargo terms","The student, R. Mitchell Lazarow, accepted the attached license on 2024-07-14 at 00:52.","The student, R. Mitchell Lazarow, submitted this Thesis for approval on 2024-07-14 at 00:59.","This Thesis was approved for publication on 2024-07-15 at 15:28.","DSpace SAF Submission Ingestion Package generated from Vireo submission #21113 on 2025-02-04 at 21:05:22","Convective activity, including thunderstorms, significantly influences Earth’s climate and environment while posing substantial risks to society. Understanding the fundamental processes driving these events is crucial, particularly given the projected increase in their occurrence and intensity. Previous studies capture impacts on precipitation occurrence and distribution but lack focus on precipitation intensity, especially at a large scale. Soil moisture affects surface heat fluxes, altering the planetary boundary layer's stability, which influences convective activity. This study examines the relationship between soil moisture and precipitation intensity across the Central United States from 2005 to 2017 using the Thunderstorm Observation by Radar (ThOR) algorithm. The analysis includes over 500,000 thunderstorm data points, correlating soil moisture with storm reflectivity and vertically integrated liquid. Findings indicate a broad negative correlation between soil moisture and precipitation intensity, suggesting that drier soils lead to stronger convective storms. Pathway variables like boundary layer height and evaporative fraction drive the mechanisms by which soil moisture influences storm intensity. The results underscore the importance of soil moisture in modulating convective storm behavior, with implications for improving forecasting and understanding of land-atmosphere interactions. Further research is needed to refine these findings and explore regional variations and other influencing factors."],"dc:format":["application/pdf"],"dc:identifier":["https://hdl.handle.net/2142/125636"],"dc:language":["en","eng"],"dc:rights":["Copyright 2024 R. Mitchell Lazarow"],"dc:subject":["Soil Moisture","Thunderstorms","Convection","Land-atmosphere Interactions","Surface Flux"],"dc:title":["A large-scale investigation of soil moisture feedbacks on precipitation intensity in the central United States"],"dc:type":["text","Thesis"],"thesis:degree_discipline":["Atmospheric Sciences"],"thesis:degree_level":["Thesis"],"thesis:degree_name":["M.S."],"thesis:institution_name":["University of Illinois at Urbana-Champaign"]},"updated_at":"2026-07-22T22:25:02Z"}