The Wisconsin’s Dynamic Influence of Shoreline Circulations on Ozone (WiscoDISCO) campaigns have explored lower atmospheric properties of the Lake Michigan shoreline during episodes of high ozone. Uncrewed aerial systems have been deployed in conjunction with Doppler lidar to study the transition of marine air as it moves from overwater to overland during lake breeze circulations. During WiscoDISCO-21 multi-platform UAS were deployed: a fixed wing UAS flew overwater and overland up to 500 m AGL to measure thermodynamic and kinematic properties of the atmosphere and a multi-rotor copter UAS flew slow ascents to capture ozone concentrations and meteorological variables over land. The lake breeze circulation was characterized by an inversion overwater with steepest inversions at 100-200 m AGL transitioning to a higher maximum inversion overland underneath which a buoyant internal boundary layer developed. Evidence for easterly circulations against synoptic flow extending up to ~450 m AGL were seen from Doppler lidar and fixed-wing UAS observations. During WiscoDISCO-22 two multirotor copters were flown simultaneously, one overwater at shoreline and one overland, to investigate the changes in ozone profiles and lower atmosphere meteorology as lake breeze circulation developed. Ozone concentrations at mid-day during lake breeze were observed at maximum concentrations above the internal boundary layer over land. Analysis of marine layer depth through computation of the height of maximum buoyancy suppression, height of maximum easterly winds and bulk Richardson number analysis will be discussed.
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Application of the NCAR FastEddy® Microscale Model to a Lake Breeze Front
This study investigates how urban environments influence boundary layer processes during the passage of a Great Salt Lake breeze using a multi-scale modeling system, NCAR’s WRF-Coupled GPU-accelerated FastEddy® (FE) model. Motivated by the need for sub-10 m scale decision support tools for uncrewed aerial systems (UAS), the FE model was used to simulate turbulent flows around urban structures at 5 m horizontal resolution with a 9 km × 9 km domain centered on the Salt Lake City International Airport. FE was one-way nested within a 1 km resolution Weather Research and Forecasting (WRF) domain spanning 400 × 400 km. Focused on the late morning lake breeze on 3 June 2022, an FE simulation was compared with WRF outputs and validated using surface and radar observations. The FE simulation revealed low sensible heat flux and cool near-surface temperatures, attributed to a relatively low specification of thermal roughness suitable for previously tested FE applications. Lake breeze characteristics were minimally affected, as FE effectively resolved interactions between the lake breeze and urban-induced turbulent eddies, providing insights into fine-scale boundary layer processes. FE’s GPU acceleration ensured efficient simulations, underscoring its potential for aiding decision support in UAS operations in complex urban environments.
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- Award ID(s):
- 2330582
- PAR ID:
- 10641473
- Publisher / Repository:
- MDPI Open Access Journal
- Date Published:
- Journal Name:
- Application of the NCAR FastEddy® microscale model to a Lake Breeze Front
- Volume:
- 15
- Issue:
- 7
- ISSN:
- 2073-4433
- Page Range / eLocation ID:
- 809
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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