Incorporating Oxygen Isotopes of Oxidized Reactive Nitrogen in the Regional Atmospheric Chemistry Mechanism, version 2 (ICOIN-RACM2)

IF 4 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
W. Walters, Masayuki Takeuchi, N. L. Ng, Meredith G. Hastings
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Abstract

Abstract. The oxygen isotope anomaly (Δ17O = δ17O − 0.52 × δ18O > 0) has proven to be a robust tool for probing photochemical cycling and atmospheric formation pathways of oxidized reactive nitrogen (NOy). Several studies have developed modeling techniques to implicitly model Δ17O of NOy molecules based on numerous assumptions that may not always be valid. Thus, these models may be oversimplified and limit our ability to compare model Δ17O values of NOy with observations. In this work, we introduce a novel method for explicitly tracking Δ17O transfer and propagation into NOy and odd oxygen (Ox), integrated into the Regional Atmospheric Chemistry Mechanism, version 2 (RACM2). Termed ICOIN-RACM2 (InCorporating Oxygen Isotopes of NOy in RACM2), this new model includes the addition of 55 new species and 729 replicate reactions to represent the propagation of Δ17O derived from O3 into NOy and Ox. Employing this mechanism within a box model, we simulate Δ17O for various NOy and Ox molecules for chamber experiments with varying initial nitrogen oxides (NOx = NO + NO2) and α-pinene conditions, revealing response shifts in Δ17O linked to distinct oxidant conditions. Furthermore, diel cycles are simulated under two summertime scenarios, representative of an urban and rural site, revealing pronounced Δ17O diurnal patterns for several NOy components and substantial Δ17O differences associated with pollution levels (urban vs. rural). Overall, the proposed mechanism offers the potential to assess NOy oxidation chemistry in chamber studies and air quality campaigns through Δ17O model comparisons against observations. The integration of this mechanism into a 3-D atmospheric chemistry transport model is expected to notably enhance our capacity to model and anticipate Δ17O across landscapes, consequently refining model representations of atmospheric chemistry and tropospheric oxidation capacity.
将氧化活性氮的氧同位素纳入区域大气化学机制第 2 版(ICOIN-RACM2)
摘要。氧同位素异常(Δ17O = δ17O - 0.52 × δ18O > 0)已被证明是探测氧化活性氮(NOy)的光化学循环和大气形成途径的有力工具。有几项研究开发了建模技术,根据许多假设隐含地模拟 NOy 分子的 Δ17O,但这些假设不一定总是有效的。因此,这些模型可能过于简化,限制了我们将 NOy 的模型 Δ17O 值与观测值进行比较的能力。在这项工作中,我们介绍了一种新方法,用于明确跟踪Δ17O 向 NOy 和奇数氧(Ox)的转移和传播,并将其集成到区域大气化学机制第 2 版(RACM2)中。这个新模型被称为 ICOIN-RACM2(在 RACM2 中纳入 NOy 的氧同位素),包括增加 55 个新物种和 729 个重复反应,以表示从 O3 派生的 Δ17O 向 NOy 和 Ox 的传播。利用箱式模型中的这一机制,我们在初始氮氧化物(NOx = NO + NO2)和α-蒎烯条件不同的箱式实验中模拟了各种 NOy 和 Ox 分子的 Δ17O,揭示了与不同氧化剂条件相关的 Δ17O的响应变化。此外,还模拟了城市和农村地区两种夏季情景下的昼夜循环,揭示了几种氮氧化物成分的明显Δ17O昼夜模式,以及与污染程度(城市与农村)相关的巨大Δ17O差异。总之,通过将Δ17O 模型与观测结果进行比较,所提出的机制为在室内研究和空气质量活动中评估 NOy 氧化化学性质提供了可能性。将这一机制整合到三维大气化学传输模式中,预计将显著提高我们模拟和预测跨地貌Δ17O 的能力,从而完善大气化学和对流层氧化能力的模式表征。
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来源期刊
Geoscientific Model Development
Geoscientific Model Development GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
8.60
自引率
9.80%
发文量
352
审稿时长
6-12 weeks
期刊介绍: Geoscientific Model Development (GMD) is an international scientific journal dedicated to the publication and public discussion of the description, development, and evaluation of numerical models of the Earth system and its components. The following manuscript types can be considered for peer-reviewed publication: * geoscientific model descriptions, from statistical models to box models to GCMs; * development and technical papers, describing developments such as new parameterizations or technical aspects of running models such as the reproducibility of results; * new methods for assessment of models, including work on developing new metrics for assessing model performance and novel ways of comparing model results with observational data; * papers describing new standard experiments for assessing model performance or novel ways of comparing model results with observational data; * model experiment descriptions, including experimental details and project protocols; * full evaluations of previously published models.
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