Abstract
This study aims to improve the performance of the Weather Research and Forecasting (WRF) model in the sea breeze circulation using the micro-Genetic Algorithm (micro-GA). We found the optimal combination of four physical parameterization schemes related to the sea breeze system, including planetary boundary layer (PBL), land surface, shortwave radiation, and longwave radiation, in the WRF model coupled with the micro-GA (WRF-μGA system). The optimization was performed with respect to surface meteorological variables (2 m temperature, 2 m relative humidity, 10 m wind speed and direction) and a vertical wind profile (wind speed and direction), simultaneously for three sea breeze cases over the northeastern coast of South Korea. The optimized set of parameterization schemes out of the WRF-μGA system includes the Mellor–Yamada–Nakanishi–Niino level-2.5 (MYNN2) for PBL, the Noah land surface model with multiple parameterization options (Noah-MP) for land surface, and the Rapid Radiative Transfer Model for GCMs (RRTMG) for both shortwave and longwave radiation. The optimized set compared with the various other sets of parameterization schemes for the sea breeze circulations showed up to 29 % for the improvement ratio in terms of the normalized RMSE considering all meteorological variables.
Highlights
Published: 26 November 2021Sea breeze is a local atmospheric circulation caused by differential heating between the sea and land surfaces in coastal regions
The resulting optimal combination of physical parameterization schemes consisted of the Mellor–Yamada–Nakanishi– Niino level-2.5 (MYNN2) planetary boundary layer (PBL) scheme, Noah-MP surface scheme, Rapid Radiative Transfer Model for GCMs (RRTMG)
The theoretical evidence for the optimal combination of the physical parameterization schemes in coastal regions is as follows: (1) The Noah-MP scheme better represented the land-surface variables leading to more realistic simulations of the sea breeze and boundary layer characteristics at coastal regions [17,58]; (2) The MYNN2 PBL scheme has been shown to more accurately reproduce the PBL structure in coastal regions [59,60,61]
Summary
Sea breeze is a local atmospheric circulation caused by differential heating between the sea and land surfaces in coastal regions. The sea breeze circulation exerts significant impacts on local weather and meteorological conditions through inland transport of moist and cool air, often bringing about development of coastal thunderstorms [3]. It plays a critical role in dispersion of low-level atmospheric pollutants by changing low-level winds and boundary layer structures [4,5]. According to a climatological study on sea Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations
Published Version (Free)
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have