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High-Resolution Simulation of Snowfall over the Korean Eastern Coastal Region Using WRF Model: Sensitivity to Domain Nesting-Down Strategy

机译:使用WRF模型的朝鲜东部沿海地区降雪的高分辨率模拟:对域嵌套策略的敏感性

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The eastern coastal area of the Korean Peninsula, Yeongdong region, often experiences severe snowfall during the winter season. We studied the development mechanism of a snowfall case occurred in February 2014 using the Weather Research and Forecasting (WRF) model at the convection-permitting resolution of 1km. The model reasonably captured the observed snowfall, and three factors were discovered as important contributors to this snowfall case: a temperature contrast between land and ocean, a high-pressure system over the northeastern part of the Korean Peninsula, and the mountainous terrain. Cold and dry air blown from the high-pressure system gains heat and moisture when it passes over the East Sea enhancing the low-level instability. When the air mass reaches the coastline, updraft is generated by the density difference with the continental atmosphere and by the mountain slope. Further sensitivity experiments were conducted by adjusting strategies of nesting down (offline and online). Sensitivity experiments consist of three offline nesting experiments with different boundary condition update frequencies in 6, 3 and 1h and one online nesting experiment that updates the boundary condition every integration time step. The major snowfall along the mountain range located in the middle of domain does not change significantly regardless of the nesting frequency. The offline nesting causes unphysical discontinuities of precipitation along the north and east sides of lateral boundary where wind blows in, which are caused by the absence of condensed hydrometeor variables in the lateral boundary condition. The domain nesting strategy tested in this study has dramatically impacted on the upper troposphere structure in the model: artificial fluctuations at the upper troposphere in the offline nesting simulations were significantly alleviated in the online nesting simulation.
机译:朝鲜半岛东部的东部沿海地区,冬季,冬季经常降雪。我们使用天气研究与预报(WRF)模型在对流允许分辨率为1km的情况下研究了2014年2月发生的降雪事件的发展机制。该模型合理地捕获了观测到的降雪,并且发现了以下三个因素是造成该降雪的重要因素:陆地和海洋之间的温度对比,朝鲜半岛东北部的高压系统以及山区。高压系统吹出的冷干空气在流经东海时会吸收热量和水分,从而增强了低水平的不稳定性。当空气质量到达海岸线时,与大陆大气的密度差和山坡会产生上升气流。通过调整向下嵌套策略(离线和在线)进行了进一步的敏感性实验。灵敏度实验包括三个离线嵌套实验,这些实验在6、3和1h内具有不同的边界条件更新频率,以及一个在线嵌套实验,该实验在每个积分时间步长更新边界条件。无论嵌套频率如何,位于区域中间的山脉沿线的主要降雪都不会发生明显变化。离线嵌套导致沿横向边界北侧和东侧吹入风的非物理性降雨中断,这是由于在横向边界条件下不存在凝结的水凝物变量而引起的。在这项研究中测试的域嵌套策略对模型的对流层上部结构产生了巨大影响:在线嵌套模拟中,离线嵌套模拟中对流层上层的人为波动得到了显着缓解。

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