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Impact of forced and internal climate variability on changes in convective environments over the eastern United States

dc.contributor.authorFranke, Megan E., author
dc.contributor.authorHurrell, James W., advisor
dc.contributor.authorRasmussen, Kristen L., committee member
dc.contributor.authorMueller, Nathan D., committee member
dc.date.accessioned2022-08-29T10:16:19Z
dc.date.available2022-08-29T10:16:19Z
dc.date.issued2022
dc.description2022 Summer.
dc.descriptionIncludes bibliographical references.
dc.description.abstractHazards from convective weather and severe storms pose a serious threat to the continental United States (CONUS). Previous studies have examined how future projected changes in climate might impact the frequency and intensity of severe weather using simulations with both convection permitting regional models and coarser-grid Earth system models. However, most of these studies have been limited to single representations of the future climate state with little insight into the uncertainty of how the population of convective storms may change. To more thoroughly explore this aspect, we utilize a large-ensemble of climate model simulations to investigate the forced response and how it may be modulated by internal variability. Specifically, we use daily data from an ensemble of 50 climate simulations with the most recent version of the Community Earth System Model (CESM) to examine changes in the severe weather environment over the eastern CONUS during boreal spring from 1870-2100. Our results indicate that the large-scale convective environment changed little between 1870 and 1990, but from then throughout the 21st century, convective available potential energy increases while 0-6 km vertical wind shear and convective inhibition decreases (increased stability). While the forced changes in these variables are robust both in space and time, we show that they are likely to be modified significantly by internal climate variability. This effect can either act to significantly enhance the forced response or conversely, suppress it in such a way that produces changes in the convective environment that are opposite to the forced response. The time evolution of bivariate distributions of convective indices illustrates that future springtime convective environments over the eastern CONUS will be characterized by relatively less frequent, but deeper and more intense convection. Future convective environments will also be less supportive of the most severe convective modes and their associated hazards.
dc.format.mediumborn digital
dc.format.mediummasters theses
dc.identifierFranke_colostate_0053N_17391.pdf
dc.identifier.urihttps://hdl.handle.net/10217/235642
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relation.ispartof2020-
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subjectinternal variability
dc.subjectstorms
dc.subjectsevere weather
dc.subjectclimate change
dc.titleImpact of forced and internal climate variability on changes in convective environments over the eastern United States
dc.typeText
dcterms.rights.dplaThis Item is protected by copyright and/or related rights (https://rightsstatements.org/vocab/InC/1.0/). You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
thesis.degree.disciplineAtmospheric Science
thesis.degree.grantorColorado State University
thesis.degree.levelMasters
thesis.degree.nameMaster of Science (M.S.)

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