About me and my work

Portrait of Kyle J. Gillett
Atmospheric Science PhD Student John D. Odegard School of Aerospace Science
University of North Dakota
Software Developer SounderPy; Weather Front

Welcome!

I'm an Atmospheric Science PhD student at the John D. Odegard School of Aerospace Science at the University of North Dakota. I also chase and document extreme weather and maintain Python software.

My Master’s thesis research at the University of North Dakota involves high-resolution numerical experiments of storm interactions that result in tornadogenesis. You'll find those details below.

My interests in meteorology primarily include severe convective storm dynamics (particularly storm interactions, tornadogenesis, & supercell behavior). I also have interests in developing data visualization tools for meteorology and weather’s impact on Great Lakes maritime disasters.



Curriculum Vitae


Publications

Oral Presentations

Posters

Research

Research focus

How rear-flank storm interactions influence supercell behavior and tornadogenesis

Comparison of tornado-like-vortex tracks in control and storm-interaction simulations
FIGURE: "Tornado-like-vortex tracks" over the course of a 6-hr simulation for (top) a control simulation of a discrete supercell and (bottom) an "interaction" simulation of the same control storm subjected to a rear-flank storm interaction. Tracks are outlined in black. The color fill is 199-min 0-1km mean simulated reflectivity.

Storm interactions are known to induce changes in parent supercell storm behavior, including the production of tornadoes (e.g., Lemon 1976; Lee et al. 2006; Hastings and Richardson 2014; Fischer and Dahl 2023; Nixon et al. 2024; Werkema et al. 2025). Why this is true remains a question often asked but generally unanswered. To address this, idealized numerical simulations are used to investigate the full three-dimensional evolution of rear-flank storm interactions (which are often associated with increased tornado production, e.g., Nixon et al. 2024). Changes in storm behavior and tornado-like vortex production are tracked and physical mechanisms governing interaction outcome are investigated.

Simulated parent supercells subjected to rear-flank storm interactions exhibited dramatic increases in tornado-like-vortex (TLV) production. In one simulation, the parent supercell's accumulated TLV duration was 35 minutes longer than the control simulation. Rear-flank downdraft (RFD) behavior also changed markedly, becoming stronger and facilitating a state of inflow-outflow balance beneath the parent's low-level updraft. These changes in RFD behavior, perhaps the most important influence of the storm interaction, appear to be driven in part by both buoyancy and dynamic mechanisms.

Comparison of simulated reflectivity evolution in control and storm-interaction simulations
FIGURE: Reflectivity evolution comparison between 0-1km simulated reflectivity (top; analogous to an average lowest-elevation WSR-88D scan height) and composite simulated reflectivity (bottom) every ten minutes starting at 170-mins.

Among the most interesting aspects of the simulated storm interactions was the fact that storm behavior appeared to change before the interaction appeared to "begin" on low-altitude simulated reflectivity. Investigating this further revealed the obvious: the storm interaction was also taking place aloft and doing so before it appeared at lower altitudes (also observed by Byers and Braham 1949, Wescott and Kennedy 1989, and Lee et al. 2006).

The simulated storm interactions start aloft as much as 15–20 minutes before appearing in low-altitude reflectivity. Composite reflectivity may serve as a tool to help identify interactions occurring aloft and perhaps increase the lead time for anticipating interaction outcomes. The interaction starting aloft also played a major role in perturbing parent storm behavior through hydrometeor seeding and several dynamic mechanisms.


Master's Thesis | University of North Dakota

Effects of a Rear-Flank Storm Interaction on Supercell Behavior and Tornado-like Vortex Development in Idealized Simulations - A Master's Thesis presented to the University of North Dakota Department of Atmospheric Science; July 2026

Committee: Dr. Catherine Finley, Dr. Bruce D. Lee, Dr. Cameron J. Nixon with special thanks to Dr. Matthew Brown, Dr. Jordan Christian, Dr. Jacob Carstens, Brandon Black, & Chris Broyles

Thesis Abstract

  • Gillett, K. J., 2026: Effects of a Rear-Flank Storm Interaction on Supercell Behavior and Tornado-like Vortex Development in Idealized Simulations. M.S. thesis, Dept. of Atmospheric Science, University of North Dakota, available at https://commons.und.edu/theses/13873/.
UND GRAD Poster Presentation
Graduate Research Achievement Day poster presenting preliminary storm-interaction findings
  • Gillett, K. J., 2026: A Numerical Investigation into the Impacts of a Rear-Flank Storm Interaction on Storm Behavior and Tornadogenesis. Poster presented at the Graduate Research Achievement Day, University of North Dakota, Grand Forks, North Dakota.

Research focus

Can tropical cyclone tornadoes be forecast before landfall using airborne observations?

Convective Environments Preceding Landfall in Tornadic Tropical Cyclones: An Analysis of Airborne Observations. Presented at the 106th AMS Annual Meeting in Houston, Texas

Advisor: Dr. Jacob D. Carstens

Plan-view figure comparing tornado-producing tropical cyclone environments
Difference fields of (a) 0-1km storm relative helicity, (b) percentage of 0-1km horizontal vorticity that is streamwise, (c) 0-3km most-unstable CAPE, and (d) surface-to-equilibrium level most-unstable CAPE, between highly-tornadic and weakly-tornadic TCs.
AMS conference poster
AMS conference poster on convective environments in tornadic tropical cyclones
  • Belzer, B. W.*, K. J. Gillett, and J. D. Carstens, 2026: Convective Environments Preceding Landfall in Tornadic Tropical Cyclones: An Analysis of Airborne Observations. Poster presented at the 106th AMS Annual Meeting, Houston, Texas, https://doi.org/10.13140/RG.2.2.29219.11047.

* denotes student coauthor

Tools

An open-source Python toolkit for retrieving, analyzing, and visualizing atmospheric sounding data.

SounderPy streamlines and unifies the path from raw sounding data to clear and advanced Skew-T and hodograph plots. The code is simple, quick, and designed for users of all experience levels.

At a glance

  • Data: RAOB and IGRAv2 observations; ACARS aircraft observations; ERA-5, RAP, RUC, & NCEP-FNL model reanalysis; HRRR, RAP, NAM, NAMNEST, GFS, SREF, and HIRESW forecast models; CM1 base-state profiles; WRF output; SHARPpy.
  • Workflow: retrieve sounding data, compute hundreds of sounding parameters, and plot data on advanced figures with only a few lines of Python or terminal commands.
  • Output: advanced sounding and hodograph visualizations.
Atmospheric sounding visualization generated with SounderPy
18z observations from OAX (Omaha, NE) on June 16th, 2014 prior to the Pilger, NE twin EF-4s; visualized with SounderPy.
Article PDF & citation
Full project abstract
Conference poster
SounderPy conference poster presented at the Central Iowa NWA Severe Storms and Doppler Radar Conference
  • Gillett, K. J., 2024: SounderPy: A Sounding Visualization Tool for Severe-Weather Analysis and Forecasting. Poster presented at the 27th Annual Central Iowa National Weather Association Severe Storms and Doppler Radar Conference, Ankeny, Iowa, https://doi.org/10.13140/RG.2.2.15823.29600.

Co-Founder, Co-Developer, Contributor to the Chase Archive Project: The web's largest storm data archive.

Resources

Origins of Updraft Rotation

What makes supercell storms "super"? The mesocyclone. This is how they form.

Updraft Helicity

Is it a cheat code? How you should actually use updraft helicity when forecasting.

Dynamics II Final Project

Review of effective-inflow-layer streamwise vorticity and storm-relative flow effects on supercell updrafts.

Space Weather Forecasting

A simple guide to forecasting the Northern Lights in the context of Auroral Substorms.

Forecasting the Witch of November

A post-event reanalysis of 9-10 November 1975 -- the Wreck of the Edmund Fitzgerald