Low-level buoyancy as a tool to characterize the atmospheric boundary layer

Date
Oct 20, 2020 2:00 PM — 3:00 PM
Location
Virtual
Low-level buoyancy as a tool to characterize the atmospheric boundary layer

Francesca Lappin is student at the OU School of Meteorology in the Masters degree program. She works as a research assistant in the Center for Autonomous Sensing and Sampling. Prior to coming to OU, she earned a BS in Meteorology from the Florida State University.

More

Abstract

Advancements in remotely piloted aircraft systems (RPAS) introduced a new way to observe the atmospheric boundary layer (ABL). Adequate sampling of the lower atmosphere is key to improving numerical weather models and understanding fine-scale processes. The ABL’s sensitivity to changes in surface fluxes leads to rapid changes in thermodynamic variables. This study proposes using low-level buoyancy to characterize ABL transitions. Previously, buoyancy has been used as a bulk parameter to quantify stability. Higher-resolution data from RPAS highlights buoyancy fluctuations. RPAS profiles from two field campaigns are used to assess the evolution of buoyancy under convective and stable boundary layers. Data from these campaigns included challenging events to forecast accurately, such as convective initiation and a low-level jet. Results show that the ABL height determined by the minimum in vertical buoyancy gradient agrees well with proven ABL height metrics, such as potential temperature gradient maxima. Moreover, in the cases presented, low-level buoyancy rapidly increases prior to convective initiation and rapidly decreases prior to the onset of a low-level jet. Low-level buoyancy is a function sensitive in space and time, and with further analysis could be used as a forecasting tool. This study expounds on the utility of buoyancy in the ABL and offers potential uses for future research.

More

Presentation

Francesca Lappin
Francesca Lappin
M.S. Student