Impact of Uncertainties in the Atmospheric Boundary Layer Height on the Numerical Simulation of Chemical Species

IF 2.3 3区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
Shuzhan Ren, Craig A. Stroud
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Abstract

Uncertainties in the atmospheric boundary layer height (ABL-H) are associated either with the uncertainties in meteorological fields or the definition of the ABL-H. When the ABL-H is involved in ABL parameterization schemes these uncertainties can have impacts on numerical simulation of chemical species. The impacts are examined numerically by employing a 1-D diffusion model with the K-profile scheme and 3-D air quality forecast model with the turbulent kinetic energy (TKE)-based scheme. The dependency on the ABL-H in the two schemes is very different. Sensitivity tests with the 1-D model show that the over-estimated/under-estimated ABL-H leads to the decrease/increase of concentration of tracers under both stable and unstable conditions due to the increase/decrease of the volume of tracers within the ABL. Under unstable conditions, the over-estimated/under-estimated ABL-H also enhances/weakens the vertical diffusivity, and leads to the decrease/increase of the concentration of tracers for the negative/positive vertical gradient of tracer. These impacts result in a little change with height within the ABL. The impacts of the ABL-H through the counter-gradient term and entrainment flux are much smaller than the impact through changing the volume of the ABL and vertical diffusivity in the ABL. Sensitivity tests with the 3-D numerical model with the TKE scheme show that over urban areas the over-estimated/under-estimated ABL-H leads to the increase/decrease of TKE in the whole ABL but does not always lead to stronger/weaker diffusivity and lower/higher concentrations of chemical species.

Abstract Image

大气边界层高度的不确定性对化学物质数值模拟的影响
大气边界层高度(ABL-H)的不确定性与气象场的不确定性或 ABL-H 的定义有关。当 ABL-H 涉及 ABL 参数化方案时,这些不确定性会对化学物种的数值模拟产生影响。通过采用 K-profile 方案的一维扩散模型和基于湍流动能 (TKE) 方案的三维空气质量预报模型,对这些影响进行了数值检验。两种方案对 ABL-H 的依赖程度大不相同。一维模型的敏感性测试表明,在稳定和不稳定条件下,高估/低估 ABL-H 都会导致示踪剂浓度的下降/上升,原因是 ABL 内示踪剂体积的增加/减少。在不稳定条件下,高估/低估的 ABL-H 也会增强/减弱垂直扩散性,并导致示踪剂垂直梯度为负/正时的示踪剂浓度下降/上升。这些影响导致 ABL 高度变化不大。ABL-H 通过反梯度项和夹带通量产生的影响远远小于通过改变 ABL 的体积和 ABL 中的垂直扩散性产生的影响。采用 TKE 方案的三维数值模式进行的敏感性测试表明,在城市地区,高估/低估 ABL-H 会导致整个 ABL 的 TKE 增加/减少,但并不总是导致扩散性增强/减弱以及化学物种浓度降低/升高。
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来源期刊
Boundary-Layer Meteorology
Boundary-Layer Meteorology 地学-气象与大气科学
CiteScore
7.50
自引率
14.00%
发文量
72
审稿时长
12 months
期刊介绍: Boundary-Layer Meteorology offers several publishing options: Research Letters, Research Articles, and Notes and Comments. The Research Letters section is designed to allow quick dissemination of new scientific findings, with an initial review period of no longer than one month. The Research Articles section offers traditional scientific papers that present results and interpretations based on substantial research studies or critical reviews of ongoing research. The Notes and Comments section comprises occasional notes and comments on specific topics with no requirement for rapid publication. Research Letters are limited in size to five journal pages, including no more than three figures, and cannot contain supplementary online material; Research Articles are generally fifteen to twenty pages in length with no more than fifteen figures; Notes and Comments are limited to ten journal pages and five figures. Authors submitting Research Letters should include within their cover letter an explanation of the need for rapid publication. More information regarding all publication formats can be found in the recent Editorial ‘Introducing Research Letters to Boundary-Layer Meteorology’.
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