Planetary Boundary Layer Flow over Complex Terrain during a Cold Surge Event: A Case Study

• Published in: Atmosphere Vol. 15; no. 2; p. 153
• Main Authors: Lee, Young-Hee, Lim, Hee-Jeong, Lee, Gyuwon
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01-01-2024
• Subjects: Adiabatic; Adiabatic flow; Air temperature; Atmospheric boundary layer; Boundary layer; Boundary layer flow; Boundary layers; Case studies; cold surges; Cold weather; Daytime; Environmental aspects; Froude number; Gravity; High resolution; Hydraulics; Ice; lee jump; Mathematical models; Microgravity; Mountains; Numerical simulations; Planetary boundary layer; Potential temperature; Radiation; Radiosonde data; Radiosondes; RGSW theory; Shallow water; Simulation; Streamlines; Terrain; Topography; Variables; Vertical profiles; Weather forecasting; Wind; Wind shear; South Korea
• ISSN: 2073-4433; 2073-4433
• DOI: 10.3390/atmos15020153

Planetary boundary layer (PBL) flow over complex terrain during a cold surge event was investigated using 3-hourly radiosonde measurements in upwind, near ridge, and downwind locations of mountains in the northeastern part of Republic of Korea and using a high-resolution (333-m) numerical simulation. A cold surge occurred on 23 January 2018 and lasted for 4 days. We analyzed onset day of the cold surge when air temperature dropped rapidly. Analysis of the radiosonde data shows that the PBL was characterized by an adiabatic layer with strong capping inversion in early morning and evening as well as during daytime in the upwind and near-ridge sites. The PBL flow at the near-ridge site was strongest among three sites except at 0600 local standard time (LST) when the PBL flow in the lee was strongest. We performed high-resolution (333-m) numerical simulations using the Weather Research and Forecasting (WRF) model. The adiabatic PBL in the upwind site at 0600 LST was simulated, although its depth was underestimated. The model reproduced the strong low-level wind at 0600 LST and large wind shear during the daytime in the lee, but it did not capture the exact timing of the large wind shear. The model showed overall good performance in simulating the vertical profile of the virtual potential temperature and wind below 2 km above ground level at the three sites, with a high index of agreement (IOA) except for the wind at 1200 and 1500 LST in the lee. To examine the cause for the different behavior of PBL flow in the lee of mountains between 0600 LST and the daytime, we calculated the Froude number for PBL flow using radiosonde measurements based on reduced gravity shallow water (RGSW) theory. At 0600 LST, the upwind Froude number F0 was close to 1, while during the daytime, it was much lower than 1. The observed lee flow behavior was consistent with the flow regime change of a single layer over an obstacle with changing F0; the flow with a propagating lee jump changes into that with a stationary lee jump with decreasing F0. Numerical simulation shows that the steepening of streamlines of lee-wave field leads to a jump-like structure in the lee of mountains during the daytime.