Simulations of Differential Reflectivity Columns in Quasi-linear Convective Systems

Much research over the past decade has revealed that dual-polarization radar is a powerful tool in furthering our understanding of severe storm dynamics and subsequently improving warning strategies for these hazardous events. However, there are currently very few studies examining a particularly prolific severe convective storm mode with dual-polarization radar: quasi-linear convective systems (QLCSs). These storms can occur in any season of the year throughout most of the contiguous United States and can have immense societal impacts. Warning for the hazards produced by QLCSs is currently a significant operational challenge, therefore, research is needed to see if applying dual-polarization radar more in warning strategies for QLCSs will help. Two novel and complementary modeling studies are presented in this dissertation that examine a particular dual-polarization signature in QLCSs: the differential reflectivity (ZDR) column. The ZDR column has been shown to likely have the most potential in anticipating tornadic potential in supercells. Additionally, the ZDR column is an updraft-associated feature and updrafts are critical for severe weather production in QLCSs. In the first study, the ZDR column is compared between two microphysics parameterization schemes and found to be more realistic in the National Severe Storms Laboratory-Double Moment scheme than the Morrison scheme. Additionally, ZDR columns are often found collocated with a strong mid-level updraft and often found at the same time with a strong low-level updraft in the vicinity. In the second study, the sensitivity of the ZDR column to low-level hodograph shape and size is examined as well as the connection between ZDR columns and low-level mesovortices. ZDR columns are largest when the low-level shear is strongest, yet there is no systematic decrease of column size with decreasing shear. ZDR columns are more likely to be found immediately rearward of a near-surface mesovortex when the low-level hodograph is straight and has large shear. However, ZDR columns away from mesovortices are often more pronounced than when in the vicinity of a mesovortex. Advisor: Matthew S. Van Den Broeke

Publication Details

Journal
Insecta mundi
Published
2025-06-01
Primary Topic
Geochemistry and Geologic Mapping
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article

Simulations of Differential Reflectivity Columns in Quasi-linear Convective Systems

Insecta mundi
Geochemistry and Geologic Mapping
article

Simulations of Differential Reflectivity Columns in Quasi-linear Convective Systems

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Abstract

Much research over the past decade has revealed that dual-polarization radar is a powerful tool in furthering our understanding of severe storm dynamics and subsequently improving warning strategies for these hazardous events. However, there are currently very few studies examining a particularly prolific severe convective storm mode with dual-polarization radar: quasi-linear convective systems (QLCSs). These storms can occur in any season of the year throughout most of the contiguous United States and can have immense societal impacts. Warning for the hazards produced by QLCSs is currently a significant operational challenge, therefore, research is needed to see if applying dual-polarization radar more in warning strategies for QLCSs will help. Two novel and complementary modeling studies are presented in this dissertation that examine a particular dual-polarization signature in QLCSs: the differential reflectivity (ZDR) column. The ZDR column has been shown to likely have the most potential in anticipating tornadic potential in supercells. Additionally, the ZDR column is an updraft-associated feature and updrafts are critical for severe weather production in QLCSs. In the first study, the ZDR column is compared between two microphysics parameterization schemes and found to be more realistic in the National Severe Storms Laboratory-Double Moment scheme than the Morrison scheme. Additionally, ZDR columns are often found collocated with a strong mid-level updraft and often found at the same time with a strong low-level updraft in the vicinity. In the second study, the sensitivity of the ZDR column to low-level hodograph shape and size is examined as well as the connection between ZDR columns and low-level mesovortices. ZDR columns are largest when the low-level shear is strongest, yet there is no systematic decrease of column size with decreasing shear. ZDR columns are more likely to be found immediately rearward of a near-surface mesovortex when the low-level hodograph is straight and has large shear. However, ZDR columns away from mesovortices are often more pronounced than when in the vicinity of a mesovortex. Advisor: Matthew S. Van Den Broeke

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Simulations of Differential Reflectivity Columns in Quasi-linear Convective Systems · Insecta mundi (2025) | TGRS Research Map | TGRS