A Numerical Simulation Of Sea Breeze Thunderstorm Structure Over The Hainan Island

The role of the sea breeze circulation, including the sea breeze front, in triggering thunderstorm has long been recognized. The afternoon thunderstorms triggered by sea breeze can affect the basic characteristics of the sea breeze and its change. In this paper, the thunderstorm caused by sea breeze is called sea breeze thunderstorm. Surrounded by the sea, Hainan Island has strong sea breeze and rich water vapor under the influence of tropical ocean. It has a high incidence of sea breeze thunderstorm, which is triggered by interaction of local circulations such as land-sea breeze and mountain-valley breeze.The WRF-ARW model (Version 3.6) coupled with the Noah land surface is used to simulate the sea breeze thunderstorm over the Hainan Island during July 20, 2012. The characteristics of thunderstorm over complex terrain are analyzed with radar, satellite, sounding and surface observations data. The structure and evolution of thunderstorm as well as its trigger mechanism are also discussed. This paper is intended to represent the mechanism of sea breeze thunderstorm and improve the forecasting performance. As a typical sea breeze thunderstorm day, there was a significant wind shift around the island. The low-level sea breeze and land cover caused a unique water vapor distribution, which provided the conditions for local thunderstorm to produce precipitation. The convective instability layer emerged in the southern part of the island, which was conducive to the formation and development of the convective activity. While the cold air in the north of island broke the unstable layer, the convection occurrence became more difficult in this region. After the sea breeze formed along the coast, it penetrated inland and developed gradually. Because of the topography forcing, northern and southern sea breezes met in the vicinity of Baoting station. As a result, a significant sea breeze convergence zone has formed, affecting local divergence and characteristics of vortex. Under the favorable dynamical condition, the local thunderstorm weather occurred. When sea breeze thunderstorm over Hainan is discussed, we should not only concern with the development of the sea breeze front, but also need to analyze the local distribution of convective inhibition. The evolution of local energy and convective parameters can indicate the arise of sea breeze thunderstorm in temporal and spatial scales. The large convective available potential energy (CAPE) and small convective inhibition (CIN) have provided favorable conditions for the development of thunderstorm before it occurred. As the occurrence of thunderstorm, the instability energy was released. The CAPE decayed rapidly and the CIN began to rise. It was a symbol that thunderstorm system has entered into the decline stage. Under the influence of the tropical ocean, the water vapor, convective potential energy and the level of free convection keep long-lasting development state which is favorable for the convection.The convection would develop autonomously when the uplift produced by sea breeze convergence overcome the convective inhibition and reach free convection level, so the sea breeze convergence can often trigger thunderstorm in Hainan. The sea breeze thunderstorm is closely related to the local terrain, which affects the spatial and temporal distributions of low-level wind and convection convergence zone. This study is conducive to understand sea breeze thunderstorm over Hainan Island and the key factor to forecast it, but we still need further studies of more cases to support the relevant conclusion.Radiation process plays an important role in the mesoscale model. To make sure the mesoscale model can accurately describe the radiation process in detail, it is necessary to take the variation of the atmospheric composition (water vapor, ozone, carbon dioxide, clouds and aerosols) and their effect on the radiation process fully into account. There exists different ways to deal with these atmospheric components in different radiation parameterization schemes, which leads to wide difference in simulation, and the results of suitable radiation parameterization scheme can be much closer to the actual situation. The WRF-ARW model (Version 3.7) coupled with the Noah land-surface process is used to simulate the sea breeze thunderstorm over the Hainan Island on July 20,2012. The characteristics of thunderstorm in different radiation experiments are analyzed with radar and surface observation data. The structure and evolution of thunderstorm as well as its trigger mechanism are also discussed. This paper is intended to study the impact of radiation parameterizations (Dudhia+RRTM and RRTMG+RRTMG) on simulated local sea breeze thunderstorm and its physical mechanism. Different radiation parameterization schemes have different ways of dealing with cloud, aerosol, and greenhouse gases in the radiative transfer process, resulting in different amount of atmospheric absorption of heat. The energy near the ground simulated by RAD experiment is less than that of CNTL, causing the land-sea thermal and pressure gradient of RAD is relatively small, at the same time, the atmosphere stratification tends to be more stable. The land-sea breeze system is a wind pattern which is generated by the differences in the heat budgets of the land and sea surfaces. In the two experiments, the land-sea thermal and pressure differences generate variation of local sea breeze intensity and location. This variation was particularly evident in the sea breeze convergence zone, where wind speed of CNTL experiment was greater than 3.0m·s-1, while the RAD was only 1.0m·s-1. The strength of sea breeze convergence will affect local divergence, characteristics of vortex, and dynamical condition, so the sea breeze simulated by CNTL is more powerful, which can provide better lifting conditions and water vapor transport for sea breeze thunderstorm. Therefore, the intensity of thunderstorm simulated by CNTL are stronger than RAD experiment.