Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

A Climatology of Cell Mergers with Supercells and Their Association with Mesocyclone Evolution

View through CrossRef
Abstract In this study, we present a climatology of observed cell mergers along the paths of 342 discrete, right-moving supercells and their association with temporal changes in low-level mesocyclone strength (measured using azimuthal shear). Nearly one-half of the examined supercells experience at least one cell merger. The frequency of cell merger occurrence varies somewhat by geographical region and the time of day. No general relationship exists between cell merger occurrence and temporal changes in low-level azimuthal shear; this corroborates prior studies in showing that the outcome of a merger is probably sensitive to storm-scale and environmental details not captured in this study. Interestingly, we find a significant inverse relationship between premerger azimuthal shear and the subsequent temporal evolution of azimuthal shear. In other words, stronger low-level mesocyclones are more likely to weaken after cell mergers and weaker low-level mesocyclones are more likely to strengthen. We also show that shorter-duration cell merger “events” (comprising multiple individual mergers) are more likely to be associated with a steady or weakening low-level mesocyclone whereas longer-duration cell merger events (3–4 individual mergers) are more likely to be associated with a strengthening low-level mesocyclone. These findings suggest what physical processes may influence the outcome of a merger in different scenarios and that the impact of these processes on low-level mesocyclone strength may change depending on storm maturity. We establish a baseline understanding of the supercell–cell merger climatology and highlight areas for future research in how to better anticipate the outcomes of cell mergers. Significance Statement A common assumption in idealized supercell simulations is that the background environment is homogeneous. Cells merging into a primary supercell represent one of many ways in which the environment might be significantly inhomogeneous. This study analyzes the paths of 342 supercells with a particular focus on how cell merger occurrence influences the strength of the low-level mesocyclone. Almost one-half of all supercells experience at least one cell merger. Supercells are more likely to weaken after a cell merger event if the premerger mesocyclone was strong or if the merger event is relatively short, and vice versa for the likelihood for a supercell to strengthen. These findings are important for those interested in short-term predictions of supercell evolution in response to cell mergers and suggest what dynamic processes may play a role in governing these relationships.
Title: A Climatology of Cell Mergers with Supercells and Their Association with Mesocyclone Evolution
Description:
Abstract In this study, we present a climatology of observed cell mergers along the paths of 342 discrete, right-moving supercells and their association with temporal changes in low-level mesocyclone strength (measured using azimuthal shear).
Nearly one-half of the examined supercells experience at least one cell merger.
The frequency of cell merger occurrence varies somewhat by geographical region and the time of day.
No general relationship exists between cell merger occurrence and temporal changes in low-level azimuthal shear; this corroborates prior studies in showing that the outcome of a merger is probably sensitive to storm-scale and environmental details not captured in this study.
Interestingly, we find a significant inverse relationship between premerger azimuthal shear and the subsequent temporal evolution of azimuthal shear.
In other words, stronger low-level mesocyclones are more likely to weaken after cell mergers and weaker low-level mesocyclones are more likely to strengthen.
We also show that shorter-duration cell merger “events” (comprising multiple individual mergers) are more likely to be associated with a steady or weakening low-level mesocyclone whereas longer-duration cell merger events (3–4 individual mergers) are more likely to be associated with a strengthening low-level mesocyclone.
These findings suggest what physical processes may influence the outcome of a merger in different scenarios and that the impact of these processes on low-level mesocyclone strength may change depending on storm maturity.
We establish a baseline understanding of the supercell–cell merger climatology and highlight areas for future research in how to better anticipate the outcomes of cell mergers.
Significance Statement A common assumption in idealized supercell simulations is that the background environment is homogeneous.
Cells merging into a primary supercell represent one of many ways in which the environment might be significantly inhomogeneous.
This study analyzes the paths of 342 supercells with a particular focus on how cell merger occurrence influences the strength of the low-level mesocyclone.
Almost one-half of all supercells experience at least one cell merger.
Supercells are more likely to weaken after a cell merger event if the premerger mesocyclone was strong or if the merger event is relatively short, and vice versa for the likelihood for a supercell to strengthen.
These findings are important for those interested in short-term predictions of supercell evolution in response to cell mergers and suggest what dynamic processes may play a role in governing these relationships.

Related Results

The Influence of Cell Mergers on Supercell Characteristics and Tornado Evolution on 27–28 April 2011
The Influence of Cell Mergers on Supercell Characteristics and Tornado Evolution on 27–28 April 2011
Abstract Numerous questions remain regarding the influence of environmental inhomogeneities on supercell evolution. Motivated by this topic, this study associates...
Observed Relationships between Supercell Mesocyclone Intensity and Evolution, Background Environmental Characteristics, and Cell Mergers
Observed Relationships between Supercell Mesocyclone Intensity and Evolution, Background Environmental Characteristics, and Cell Mergers
Abstract Cell mergers with supercells are relatively common, but much remains unknown about how they may influence subsequent supercell hazards. Furthermore, many outstanding quest...
What is a Mesocyclone?
What is a Mesocyclone?
<p>A defining feature of supercells is the <em>mesocyclone</em>, which has been implicated in facilitating updraft maintenance and strengt...
Characterization of thunderstorms to detect, track and extrapolate supercells.
Characterization of thunderstorms to detect, track and extrapolate supercells.
Supercells represent a major safety issue due to violent phenomena they can provoke, such as large hail, severe wind gust, heavy rain and, sometimes, tornadoes.That’s why this issu...
Supercell low-level mesocyclones: Origins of inflow and vorticity
Supercell low-level mesocyclones: Origins of inflow and vorticity
<p>In this presentation, we will recap the historical use of storm-relative helicity in supercell environments, share updated climatioglical distributions from both t...
Complex Collision Tumors: A Systematic Review
Complex Collision Tumors: A Systematic Review
Abstract Introduction: A collision tumor consists of two distinct neoplastic components located within the same organ, separated by stromal tissue, without histological intermixing...
Frequency of Common Chromosomal Abnormalities in Patients with Idiopathic Acquired Aplastic Anemia
Frequency of Common Chromosomal Abnormalities in Patients with Idiopathic Acquired Aplastic Anemia
Objective: To determine the frequency of common chromosomal aberrations in local population idiopathic determine the frequency of common chromosomal aberrations in local population...

Back to Top