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University of Illinois Urbana-Champaign

Orographic and thermodynamic processes influencing mixed-phase precipitation banding in an eastern United States winter storm

Abstract

dc:description

Mesoscale snowbands within the comma head of wintertime extratropical cyclones can cause major societal disruptions and are challenging to predict. Previous literature has suggested the importance of mid-level frontogenesis in primary snowband development northwest of the surface low. However, little is known about the coupled microphysical and thermodynamic processes within these primary snowbands. In this study we examine the 16–17 January 2022 winter storm, where complex terrain interacted with a near-freezing thermodynamic profile to support a heavy mixed-phase precipitation band over western New York. Microphysical observations for this case were obtained from the University of Illinois System for Characterizing and Measuring Precipitation (SCAMP), a multi-sensor suite of instruments deployed in Buffalo, NY. To further investigate the orographic and thermodynamic processes influencing the mixed precipitation band, output from a Weather Research and Forecasting (WRF) model simulation with 1 km grid spacing was analyzed. Simulated WRF vertical cross sections through the banded precipitation revealed mid-level ascent above persistent low-level subsidence. This low-level subsidence initially formed over the higher terrain southeast of Buffalo, NY in a stable layer with orographic gravity waves. Within this subsidence layer, adiabatic warming allowed for an isolated pocket of above-freezing temperatures to form, which then moved northwest toward the SCAMP site in Buffalo, NY. As the above-freezing layer developed, particle size and fall speed distributions from the SCAMP depicted melting snow as the predominant precipitation type. Overall, the orographic gravity waves and associated adiabatic warming promoted snow particle melting, and consequently, the intense snowfall rates observed within the primary snowband during this storm.

Degree

thesis:*
Name thesis:degree_name
M.S.
Level thesis:degree_level
Thesis
Discipline thesis:degree_discipline
Atmospheric Sciences
Grantor
University of Illinois Urbana-Champaign
Year dc:date
2025

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Jesmonth, Kaitlyn R.
Contributors dc:contributor
  • Nesbitt, Stephen
  • Rauber, Robert
  • Steenburgh, Jim

Subjects

dc:subject × 5

Rights

dc:rights
Statement dc:rights
  • Copyright 2025 Kaitlyn Jesmonth
Language dc:language
en, eng

Identifiers

dc:identifier.*
Handle dc:identifier
https://hdl.handle.net/2142/129296

Chain of custody

source
Harvested from
University of Illinois - Urbana-Champaign
Base URL
www.ideals.illinois.edu/oai-pmh
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
citation

Jesmonth, Kaitlyn R.. Orographic and thermodynamic processes influencing mixed-phase precipitation banding in an eastern United States winter storm. Thesis thesis, University of Illinois Urbana-Champaign, 2025. https://hdl.handle.net/2142/129296