High-Resolution Modeling of Mesoscale Circulation in the Atmospheric Boundary Layer over a Complex Coastal Area
Abstract
:1. Introduction
2. Materials and Methods
2.1. Site Description and Observations
2.2. Model Description
2.3. Evaluation
2.4. Sea-Breeze Characteristics
- Onset (LST): The onset is the time when the sea-breeze front (SBF) passes. The time of SBF passage is defined as the time when the wind direction at 10 m AGL changes from offshore or weak wind (wind speed ≤ 1.5 m s−1) to onshore flow (60°–240°) after sunrise, and when the change in wind direction is greater than 30° over the course of an hour;
- Cessation (LST): The cessation is the time when the sea breeze ends. The cessation happens when the wind speed at 10 m AGL is ≤1.5 m s−1, or when the wind is an offshore flow between 15:00 and 24:00 LST. Before offshore flow, the previous wind must be blown onshore;
- Depth of sea breeze: The depth of onshore flow with a speed ≥1.5 m s−1;
- Intensity of sea breeze: The wind speed of the sea breeze.
- We calculate the sea-breeze characteristics by using 10-minute moving-average data for both simulation and observation.
2.5. Design of Sensitivity Experiment
3. Observations and Model Evaluation
3.1. General Meteorological Conditions for 15 July 2018
3.2. Model Evaluation
4. Analysis of Numerical Simulation and Discussion
4.1. Regional-Scale Description of the Flows
4.2. Down-Valley Wind and Sea Breeze at BSWO
4.3. Sensitivity of Simulated Flow Structure to Model Resolution
5. Summary
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Domains | D01 | D02 | D03 | D04 |
---|---|---|---|---|
Horizontal resolution (m) | 9000 | 3000 | 1000 | 333 |
Horizontal grid | 181 × 181 | 163 × 163 | 163 × 163 | 210 × 210 |
Microphysics | WRF double-moment 6-class scheme | |||
Surface layer | Revised MM5 Monin–Obukhov scheme | |||
Land surface | Unified Noah land surface model | |||
Longwave radiation | Rapid radiative transfer model scheme | |||
Shortwave radiation | Dudhia scheme | |||
Boundary layer | Shin–Hong scale-aware PBL scheme | |||
Cumulus | Multiscale Kain–Fritsch scheme | - | - | - |
Experiment | Horizontal Resolution (m) | Vertical Resolution (Levels) |
---|---|---|
S03 | 1000 | 60 |
S03V | 1000 | 68 |
S04 | 333 | 60 |
S04V (Default) | 333 | 68 |
N | 2-m Air Temperature | 10-m Wind Speed | 10-m Wind Vector | |||||
---|---|---|---|---|---|---|---|---|
MBE (K) | RMSE (K) | IOA | MBE (m s−1) | RMSE (m s−1) | IOA | RMSEu,v (m s−1) | IOAu,v | |
360 | −0.43 | 1.28 | 0.95 | 0.91 | 1.56 | 0.62 | 2.22 | 0.71 |
Time (LST) | N | Virtual Potential Temperature | Wind Speed | Wind Vector | |||||
---|---|---|---|---|---|---|---|---|---|
MBE (K) | RMSE (K) | IOA | MBE (m s−1) | RMSE (m s−1) | IOA | RMSEu,v (m s−1) | IOAu,v | ||
0530 | 20 | −0.34 | 0.65 | 0.99 | 0.39 | 1.16 | 0.51 | 1.51 | 0.86 |
0830 | 20 | −0.04 | 0.36 | 0.99 | 1.03 | 1.68 | 0.42 | 2.29 | 0.62 |
1130 | 20 | −1.08 | 1.22 | 0.85 | 0.54 | 0.92 | 0.74 | 1.55 | 0.91 |
1430 | 20 | −1.13 | 1.18 | 0.74 | 0.41 | 0.97 | 0.89 | 1.3 | 0.92 |
1730 | 20 | −1.29 | 1.36 | 0.81 | 0.82 | 1.55 | 0.20 | 1.95 | 0.73 |
Variables | S04V | S04 | S03V | S03 |
---|---|---|---|---|
Onset (LST) | 1011 | 1207 | 0951 | 1257 |
Cessation (LST) | 1836 | 1707 | 1902 | 1912 |
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Lim, H.-J.; Lee, Y.-H. High-Resolution Modeling of Mesoscale Circulation in the Atmospheric Boundary Layer over a Complex Coastal Area. Atmosphere 2021, 12, 1649. https://doi.org/10.3390/atmos12121649
Lim H-J, Lee Y-H. High-Resolution Modeling of Mesoscale Circulation in the Atmospheric Boundary Layer over a Complex Coastal Area. Atmosphere. 2021; 12(12):1649. https://doi.org/10.3390/atmos12121649
Chicago/Turabian StyleLim, Hee-Jeong, and Young-Hee Lee. 2021. "High-Resolution Modeling of Mesoscale Circulation in the Atmospheric Boundary Layer over a Complex Coastal Area" Atmosphere 12, no. 12: 1649. https://doi.org/10.3390/atmos12121649