Spatial Variability in the Diurnal Evolution of Planetary Boundary Layer Heights in a Coastal-Urban Environment

Date
Nov 18, 2024 3:30 PM — 4:20 PM
Location
NWC 1350 and Google Meet
Speaker
Michelle Spencer
Spatial Variability in the Diurnal Evolution of Planetary Boundary Layer Heights in a Coastal-Urban Environment

Michelle is a PhD student working with Drs. Petra Klein and Elizabeth Smith. She earned prior degrees at UW-Milwaukee and Metropolitan State University-Denver. She focuses on boundary layer properities in the urban-coastal interface as part of the DOE-AWAKEN project under the OU-NSSL collaboratic CUBIC project.

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Abstract

The planetary boundary layer (PBL) height is a crucial parameter that determines the vertical extent of turbulent mixing, which is important for several meteorological applications such as air quality forecasting and convective cloud modeling. Knowledge of how PBL heights vary across coastal-urban environments is limited, as many past studies of PBL height occur at point locations for one city/place, are limited by coarse temporal resolution (e.g. twice daily radiosondes), or rely on model reanalyses with known biases and coarse spatial resolutions. This study investigates the spatial heterogeneity of PBL heights across the complex Houston- Galveston region, focusing on the effects of different characteristics and processes on the diurnal evolution of the PBL height. The Coastal Urban Boundary-layer Interactions with Convection (CUBIC) field campaign provides a unique dataset, consisting of continuous thermodynamic and kinematic observations through the depth of the PBL at t hree distinct locations. PBL heights are estimated via a fuzzy logic algorithm that combines Doppler lidar, Atmospheric Emitted Radiance Interferometer (AERI), and microwave radiometer data for each day at a 10-minute resolution. Results indicate substantial differences between the three locations and considerable variation, with urban PBL heights consistently deeper than the rural and coastal locations. Additionally, there are distinct differences in PBL height on sea breeze days versus non-sea breeze days. This study’s findings highlight the presence of small- scale variability within the PBL and indicate a need for further exploration of PBL variability in spatially heterogeneous and complex areas to better understand the processes at play. Disentangling the PBL characteristics driving the observed variability of the PBL heights is important for future model parameterization development, air quality forecasting, and convective modeling.

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Presentation

Michelle R. Spencer
Michelle R. Spencer
Ph.D. Student

I started my PhD journey here at OU as a graduate research assistant in January 2022. My work includes investigating boundary layer interactions around Houston, TX and how the sea-breeze and air pollution may affect convection initiation surrounding the city. I focus on ground-based boundary layer profiler observations. Prior to OU, I received my M.S. in Atmospheric Sciences from the University of Wisconsin-Milwaukee, where I focused on a modeling study investigating forecast uncertainty in high-shear low-CAPE environments in the southeastern United States relating to sea-surface temperature sensitivities. I earned my B.S. in Meteorology from the Metropolitan State University of Denver in December 2019.