How Do Planetary Boundary Layer Schemes Perform in PM2.5-O3 Composite Pollution in the Beijing-Tianjin-Hebei (BTH)? An In-Depth Mechanism Analysis From the Underlying Code

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Wenxing Jia, Xiaoye Zhang, Yi Lin, Deying Wang, Hong Wang, Yaqiang Wang
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Abstract

Parameterization schemes undergo continuous updates, with most refinements documented in code implementations, necessitating in-depth code analysis for evaluation. Focusing on PM2.5-O3 composite pollution in the Beijing-Tianjin-Hebei region, 10 planetary boundary layer (PBL) schemes were evaluated for their simulation performance. The 2-m temperature (T2) demonstrates daytime dependence on temperature gradient and transport coefficient, shifting to surface temperature dominance at night. Saturated mixing ratio predominantly governs 2-m relative humidity (RH2) variations, while 10-m wind speed (WS10) derives from the first-level wind speed. Vertical profile comparisons reveal degraded simulation accuracy at lower levels, attributed to human activities’ influences within the PBL. The total energy-mass flux scheme exhibited distinct deviations due to failure to recognize the existence of shallow cumulus, consequently suppressing vertical mixing. Turbulent diffusion coefficient (K) discrepancies in nonlocal closure schemes primarily stem from PBL height (PBLH) variations, whereas local closure schemes show mixing length dominance (∼63%). Dissipation rate considerations exert stronger impacts at lower levels. For hybrid schemes, K calculated by Monin-Obukhov similarity theory shows enhanced magnitudes during daytime. Statistical analysis indicates the Mellor-Yamada-Janjić scheme's minor T2 deficiencies become insignificant when weighed against its superior vertical profiles of T, RH, and WS10. These insights offer critical references for PBL scheme optimization.

Abstract Image

行星边界层方案对京津冀地区PM2.5-O3复合污染的影响从底层代码进行深入的机制分析
参数化方案经历了不断的更新,在代码实现中记录了大多数改进,需要深入的代码分析来进行评估。以京津冀地区PM2.5-O3复合污染为研究对象,对10种行星边界层(PBL)方案的模拟性能进行了评价。2 m温度(T2)表现出白天对温度梯度和输运系数的依赖,夜间转向地表温度主导。饱和混合比主要支配2 m相对湿度(RH2)的变化,10 m风速(WS10)主要来源于一级风速。垂直剖面比较显示,由于人类活动在边界层内的影响,较低水平的模拟精度下降。由于不能识别浅积云的存在,总能量-质量通量方案表现出明显的偏差,从而抑制了垂直混合。非局部闭合方案中的湍流扩散系数(K)差异主要源于PBL高度(PBLH)的变化,而局部闭合方案显示混合长度优势(约63%)。在较低的水平上,耗散率的影响更大。对于混合方案,由Monin-Obukhov相似理论计算的K值在白天增大。统计分析表明,mellor - yamada - janjiki方案较小的T2缺陷在权衡其优越的T、RH和WS10垂直剖面时变得微不足道。这些见解为PBL方案优化提供了重要参考。
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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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