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Enabling high-performance cloud computing for the Community Multiscale Air Quality Model (CMAQ) version 5.3.3: performance evaluation and benefits for the user community. 为社区多尺度空气质量模型(CMAQ)5.3.3 版启用高性能云计算:性能评估及对用户社区的益处。
IF 4 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-09-19 DOI: 10.5194/gmd-17-7001-2024
Christos I Efstathiou, Elizabeth Adams, Carlie J Coats, Robert Zelt, Mark Reed, John McGee, Kristen M Foley, Fahim I Sidi, David C Wong, Steven Fine, Saravanan Arunachalam

The Community Multiscale Air Quality Model (CMAQ) is a local- to hemispheric-scale numerical air quality modeling system developed by the U.S. Environmental Protection Agency (USEPA) and supported by the Community Modeling and Analysis System (CMAS) center. CMAQ is used for regulatory purposes by the USEPA program offices and state and local air agencies and is also widely used by the broader global research community to simulate and understand complex air quality processes and for computational environmental fate and transport and climate and health impact studies. Leveraging state-of-the-science cloud computing resources for high-performance computing (HPC) applications, CMAQ is now available as a fully tested, publicly available technology stack (HPC cluster and software stack) for two major cloud service providers (CSPs). Specifically, CMAQ configurations and supporting materials have been developed for use on their HPC clusters, including extensive online documentation, tutorials and guidelines to scale and optimize air quality simulations using their services. These resources allow modelers to rapidly bring together CMAQ, cloud-hosted datasets, and visualization and evaluation tools on ephemeral clusters that can be deployed quickly and reliably worldwide. Described here are considerations in CMAQ version 5.3.3 cloud use and the supported resources for each CSP, presented through a benchmark application suite that was developed as an example of a typical simulation for testing and verifying components of the modeling system. The outcomes of this effort are to provide findings from performing CMAQ simulations on the cloud using popular vendor-provided resources, to enable the user community to adapt this for their own needs, and to identify specific areas of potential optimization with respect to storage and compute architectures.

社区多尺度空气质量模型(CMAQ)是由美国环境保护局(USEPA)开发的地方到半球尺度的空气质量数值模型系统,由社区建模与分析系统(CMAS)中心提供支持。CMAQ 被美国环保署项目办公室、州和地方空气机构用于监管目的,同时也被更广泛的全球研究界用于模拟和了解复杂的空气质量过程,以及计算环境归宿和迁移、气候和健康影响研究。利用用于高性能计算(HPC)应用的科学云计算资源,CMAQ现已作为经过全面测试的公开可用技术堆栈(HPC集群和软件堆栈)提供给两大云服务提供商(CSP)。具体来说,CMAQ配置和辅助材料已开发完成,可在其高性能计算集群上使用,包括大量在线文档、教程和指南,以便使用其服务扩展和优化空气质量模拟。通过这些资源,建模人员可以将 CMAQ、云托管数据集以及可视化和评估工具快速整合到可在全球范围内快速可靠部署的短暂集群上。本文介绍了 CMAQ 5.3.3 版云使用中的注意事项以及每个 CSP 的支持资源,并通过一个基准应用套件进行了介绍,该套件是作为测试和验证建模系统组件的典型模拟示例而开发的。这项工作的成果是提供使用流行供应商提供的资源在云上执行 CMAQ 仿真的结果,使用户社区能够根据自身需求进行调整,并确定在存储和计算架构方面可能进行优化的具体领域。
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引用次数: 0
Impacts of updated reaction kinetics on the global GEOS-Chem simulation of atmospheric chemistry. 更新反应动力学对全球 GEOS-Chem 大气化学模拟的影响。
IF 5.1 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-02-20 DOI: 10.5194/gmd-17-1511-2024
Kelvin H Bates, Mathew J Evans, Barron H Henderson, Daniel J Jacob

We updated the chemical mechanism of the GEOS-Chem global 3-D model of atmospheric chemistry to include new recommendations from the NASA Jet Propulsion Laboratory (JPL) chemical kinetics Data Evaluation 19-5 and from the International Union of Pure and Applied Chemistry (IUPAC) and to balance carbon and nitrogen. We examined the impact of these updates on the GEOS-Chem version 14.0.1 simulation. Notable changes include 11 updates to reactions of reactive nitrogen species, resulting in a 7% net increase in the stratospheric NOx (NO + NO2) burden; an updated CO + OH rate formula leading to a 2.7% reduction in total tropospheric CO; adjustments to the rate coefficient and branching ratios of propane + OH, leading to reduced tropospheric propane (-17%) and increased acetone (+3.5%) burdens; a 41% increase in the tropospheric burden of peroxyacetic acid due to a decrease in the rate coefficient for its reaction with OH, further contributing to reductions in peroxyacetyl nitrate (PAN; -3.8%) and acetic acid (-3.4%); and a number of minor adjustments to halogen radical cycling. Changes to the global tropospheric burdens of other species include -0.7% for ozone, +0.3% for OH (-0.4% for methane lifetime against oxidation by tropospheric OH), +0.8% for formaldehyde, and -1.7% for NOx. The updated mechanism reflects the current state of the science, including complex chemical dependencies of key atmospheric species on temperature, pressure, and concentrations of other compounds. The improved conservation of carbon and nitrogen will facilitate future studies of their overall atmospheric budgets.

我们更新了 GEOS-Chem 全球大气化学三维模型的化学机制,纳入了美国宇航局喷气推进实验室(JPL)化学动力学数据评估 19-5 和国际纯粹与应用化学联合会(IUPAC)的新建议,并平衡了碳和氮。我们研究了这些更新对 GEOS-Chem 14.0.1 版模拟的影响。值得注意的变化包括:对活性氮物种反应进行了 11 次更新,导致平流层氮氧化物(NO + NO2)负担净增加 7%;更新了 CO + OH 的速率公式,导致对流层 CO 总量减少 2.7%;调整了丙烷 + OH 的速率系数和支化比,导致对流层丙烷负担减少(-17%),丙酮负担增加(+3.5%);由于过氧乙酸与 OH 反应的速率系数降低,对流层中的过氧乙酸负荷增加了 41%,进一步导致过氧乙酰硝酸(PAN;-3.8%)和乙酸(-3.4%)的减少;以及对卤素自由基循环的一些微小调整。其他物种在全球对流层负担中的变化包括:臭氧-0.7%、OH +0.3%(甲烷在对流层 OH 氧化作用下的寿命-0.4%)、甲醛 +0.8%、氮氧化物-1.7%。更新后的机制反映了当前的科学水平,包括大气中关键物种对温度、压力和其他化合物浓度的复杂化学依赖性。改进后的碳和氮的保存情况将有助于今后对它们在大气中的总体预算进行研究。
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引用次数: 0
Development of inter-grid-cell lateral unsaturated and saturated flow model in the E3SM Land Model (v2.0) 在 E3SM 陆地模型(v2.0)中开发网格间横向非饱和与饱和水流模型
IF 5.1 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-10 DOI: 10.5194/gmd-17-143-2024
Han Qiu, G. Bisht, Lingcheng Li, D. Hao, Donghui Xu
Abstract. The lateral transport of water in the subsurface is important in modulating terrestrial water energy distribution. Although a few land surface models have recently included lateral saturated flow within and across grid cells, it is not a default configuration in the Climate Model Intercomparison Project version 6 experiments. In this work, we developed the lateral subsurface flow model within both unsaturated and saturated zones in the Energy Exascale Earth System Model (E3SM) Land Model version 2 (ELMv2.0). The new model, called ELMlat, was benchmarked against PFLOTRAN, a 3D subsurface flow and transport model, for three idealized hillslopes that included a convergent hillslope, divergent hillslope, and tilted V-shaped hillslope with variably saturated initial conditions. ELMlat showed comparable performance against PFLOTRAN in terms of capturing the dynamics of soil moisture and groundwater table for the three benchmark hillslope problems. Specifically, the mean absolute errors (MAEs) of the soil moisture in the top 10 layers between ELMlat and PFLOTRAN were within 1 %±3 %, and the MAEs of water table depth were within ±0.2 m. Next, ELMlat was applied to the Little Washita experimental watershed to assess its prediction of groundwater table, soil moisture, and soil temperature. The spatial pattern of simulated groundwater table depth agreed well with the global groundwater table benchmark dataset generated from a global model calibrated with long-term observations. The effects of lateral groundwater flow on the energy flux partitioning were more prominent in lowland areas with shallower groundwater tables, where the difference in simulated annual surface soil temperature could reach 0.3–0.4 ∘C between ELMv2.0 and ELMlat. Incorporating lateral subsurface flow in ELM improves the representation of the subsurface hydrology, which will provide a good basis for future large-scale applications.
摘要地下水的横向输送对调节陆地水能分布非常重要。虽然最近有一些陆表模式包含了网格单元内和网格单元间的横向饱和流,但它并不是气候模式相互比较项目第 6 版实验的默认配置。在这项工作中,我们在能源超大规模地球系统模式(E3SM)陆地模式第 2 版(ELMv2.0)中开发了非饱和区和饱和区内的横向地下流动模型。新模型名为 ELMlat,以三维地下流动和传输模型 PFLOTRAN 为基准,对三个理想化山坡进行了测试,其中包括具有不同饱和初始条件的收敛山坡、发散山坡和倾斜 V 型山坡。在捕捉三个基准山坡问题的土壤水分和地下水位动态方面,ELMlat 的性能与 PFLOTRAN 相当。具体而言,ELMlat 和 PFLOTRAN 对顶层 10 层土壤水分的平均绝对误差(MAEs)在 1 %±3 % 之间,对地下水位深度的平均绝对误差(MAEs)在 ±0.2 m 之间。接下来,将 ELMlat 应用于 Little Washita 实验流域,以评估其对地下水位、土壤水分和土壤温度的预测。模拟地下水位深度的空间模式与根据长期观测数据校准的全球模型生成的全球地下水位基准数据集非常吻合。在地下水位较浅的低洼地区,横向地下水流对能量通量分配的影响更为突出,ELMv2.0 和 ELMlat 模拟的年地表土壤温度相差可达 0.3-0.4 ∘C。在 ELM 中纳入地下横向流改进了地下水文的表示,这将为未来的大规模应用奠定良好的基础。
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引用次数: 0
Understanding changes in cloud simulations from E3SM version 1 to version 2 了解云模拟从 E3SM 版本 1 到版本 2 的变化
IF 5.1 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-10 DOI: 10.5194/gmd-17-169-2024
Yuying Zhang, Shaocheng Xie, Yi Qin, Wuyin Lin, J. Golaz, Xue Zheng, Po-Lun Ma, Yun Qian, Qi Tang, Christopher R. Terai, Meng Zhang
Abstract. This study documents clouds simulated by the Energy Exascale Earth System Model (E3SM) version 2 (E3SMv2) and attempts to understand what causes the model behavior change in clouds relative to E3SMv1. This is done by analyzing the last 30-year (1985–2014) data from the 165-year historical simulations using E3SMv1 and v2 and four sensitivity tests to isolate the impact of changes in model parameter choices in its turbulence, shallow convection, and cloud macrophysics parameterization (Cloud Layers Unified By Binormals, CLUBB); microphysical parameterization (MG2); and deep-convection scheme (ZM), as well as model physics changes in convective triggering. It is shown that E3SMv2 significantly improves the simulation of subtropical coastal stratocumulus clouds and clouds with optical depth larger than 3.6 over the stratocumulus-to-cumulus transition regimes, where the shortwave cloud radiative effect (SWCRE) is also improved, and the Southern Ocean (SO) while seeing an overall slight degradation in low clouds over other tropical and subtropical oceans. The better performance in E3SMv1 over those regions is partially due to error compensation between its simulated optically thin and intermediate low clouds for which E3SMv2 actually improves simulation of optically intermediate low clouds. Sensitivity tests indicate that the changes in low clouds are primarily due to the tuning done in CLUBB. The impact of the ZM tuning is mainly on optically intermediate and thick high clouds, contributing to an improved SWCRE and longwave cloud radiative effect (LWCRE). The impact of the MG2 tuning and the new convective trigger is primarily on the high latitudes and the SO. They have a relatively smaller impact on clouds than CLUBB tuning and ZM tuning do. This study offers additional insights into clouds simulated in E3SMv2 by utilizing multiple data sets and the Cloud Feedback Model Intercomparison Project (CFMIP) Observation Simulator Package (COSP) diagnostic tool as well as sensitivity tests. The improved understanding will benefit future E3SM developments.
摘要本研究记录了能源超大规模地球系统模式(ESM)第 2 版(ESMv2)模拟的云层,并试图了解与 E3SMv1 相比,导致云层模型行为变化的原因。具体做法是分析使用 E3SMv1 和 v2 进行的 165 年历史模拟中最近 30 年(1985-2014 年)的数据,并进行四项敏感性测试,以隔离模型参数选择变化在湍流、浅对流和云宏观物理参数化(云层统一二项式,CLUBB)、微观物理参数化(MG2)和深对流方案(ZM)方面的影响,以及模型物理在对流触发方面的变化。结果表明,ESMv2 显著改善了亚热带沿岸层积云和光学深度大于 3.6 的层积云向积云过渡区云的模拟,其中短波云辐射效应(SWCRE)也得到了改善,并改善了南大洋(SO)的模拟,但其他热带和亚热带海洋低云的模拟总体上略有下降。E3SMv1 在这些地区表现较好的部分原因是其模拟的光学稀薄低云和中间低云之间的误差补偿,而 E3SMv2 实际上改进了对光学中间低云的模拟。灵敏度测试表明,低云的变化主要是由于 CLUBB 的调整造成的。ZM 调整的影响主要是光学中间云和厚高云,有助于改善 SWCRE 和长波云辐射效应 (LWCRE)。MG2 调整和新的对流触发主要对高纬度和 SO 有影响。与 CLUBB 调整和 ZM 调整相比,它们对云的影响相对较小。本研究通过利用多个数据集和云反馈模式相互比较项目(CFMIP)观测模拟器包(COSP)诊断工具以及灵敏度测试,对 E3SMv2 模拟的云层有了更深入的了解。加深了解将有利于未来 E3SM 的开发。
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引用次数: 1
The wave-age-dependent stress parameterisation (WASP) for momentum and heat turbulent fluxes at sea in SURFEX v8.1 SURFEX v8.1 中用于海上动量和热量湍流的波龄应力参数化 (WASP)
IF 5.1 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-09 DOI: 10.5194/gmd-17-117-2024
M. Bouin, C. Lebeaupin Brossier, S. Malardel, A. Voldoire, C. Sauvage
Abstract. A widely applicable parameterisation of turbulent heat and momentum fluxes at sea has been developed for the SURFEX v8.1 surface model. This wave-age-dependent stress parameterisation (WASP) combines a close fit to available in situ observations at sea up to wind speed of 60 m s−1 with the possibility of activating the impact of wave growth on the wind stress. It aims in particular at representing the effect of surface processes that depend on the surface wind according to the state of the art. It can be used with the different atmospheric models coupled with the surface model SURFEX, including the CNRM-CM climate model, the operational (numerical weather prediction) systems in use at Météo-France, and the research model Meso-NH. Designed to be used in coupled or forced mode with a wave model, it can also be used in an atmosphere-only configuration. It has been validated and tested in several case studies covering different surface conditions known to be sensitive to the representation of surface turbulent fluxes: (i) the impact of a sea surface temperature (SST) front on low-level flow by weak wind, (ii) the simulation of a Mediterranean heavy precipitating event where waves are known to influence the low-level wind and displace precipitation, (iii) several tropical cyclones, and (iv) a climate run over 35 years. It shows skills comparable to or better than the different parameterisations in use in SURFEX v8.1 so far.
摘要为 SURFEX v8.1 地表模式开发了一种广泛适用的海上湍流热通量和动量通量参数化。这种与波浪年龄相关的应力参数化(WASP)既与风速为 60 米/秒-1 时的海上现场观测数据密切吻合,又可以激活波浪增长对风应力的影响。根据目前的技术水平,它的目的尤其在于表示取决于表面风的表面过程的影响。它可以与 SURFEX 地表模式耦合的不同大气模式一起使用,包括 CNRM-CM 气候模式、法国气象局使用的业务(数值天气预报)系统和 Meso-NH 研究模式。该模型设计用于与波浪模型耦合或强制模式,也可用于纯大气配置。它已在几个案例研究中进行了验证和测试,这些案例研究涵盖了已知对表面湍流通量表示敏感的不同表面条件:(i) 海面温度(SST)前沿对弱风低层流的影响,(ii) 地中海强降水事件模拟,已知波浪会影响低层风并使降水位移,(iii) 几个热带气旋,以及 (iv) 35 年的气候运行。它所显示的技能与迄今为止 SURFEX v8.1 中使用的不同参数相当或更好。
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引用次数: 0
WRF (v4.0)–SUEWS (v2018c) coupled system: development, evaluation and application WRF(v4.0)-SUEWS(v2018c)耦合系统:开发、评估和应用
IF 5.1 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-09 DOI: 10.5194/gmd-17-91-2024
Ting Sun, H. Omidvar, Zhenkun Li, Ning Zhang, Wenjuan Huang, S. Kotthaus, H. C. Ward, Zhiwen Luo, S. Grimmond
Abstract. The process of coupling the Surface Urban Energy and Water Scheme (SUEWS) into the Weather Research and Forecasting (WRF) model is presented, including pre-processing of model parameters to represent spatial variability in surface characteristics. Fluxes and mixed-layer height observations in the southern UK are used to evaluate a 2-week period in each season. Mean absolute errors, based on all periods, are smaller in residential Swindon than central London for turbulent sensible and latent heat fluxes (QH, QE) with greater skill on clear-sky days on both sites (for incoming and outgoing short- and long-wave radiation, QH and QE). Clear-sky seasonality is seen in the model performance: there is better absolute skill for QH and QE in autumn and winter, when there is a higher frequency of clear-sky days, than in spring and summer. As the WRF-modelled incoming short-wave radiation has large errors, we apply a bulk transmissivity derived from local observations to reduce the incoming short-wave radiation input to the land surface scheme – this could correspond to increased presence of aerosols in cities. We use the coupled WRF–SUEWS system to investigate impacts of the anthropogenic heat flux emissions on boundary layer dynamics by comparing areas with contrasting human activities (central–commercial and residential areas) in Greater London – larger anthropogenic heat emissions not only elevate the mixed-layer heights but also lead to a warmer and drier near-surface atmosphere.
摘要介绍了将地表城市能量和水计划(SUEWS)与天气研究和预报(WRF)模式耦合的过程,包括模式参数的预处理,以表示地表特征的空间变化。英国南部的通量和混合层高度观测数据用于评估每个季节的两周时间。在所有时段,斯温顿住宅区的湍流显热通量和潜热通量(QH、QE)的平均绝对误差小于伦敦市中心,两个地点晴天时的误差更大(入射和出射短波和长波辐射、QH 和 QE)。晴朗天气的季节性表现在模型性能上:秋冬季晴朗天气频率较高,QH 和 QE 的绝对技能优于春夏季。由于 WRF 模拟的入射短波辐射误差较大,我们采用了从当地观测数据中得出的体透射率,以减少输入陆地表面方案的入射短波辐射--这可能与城市中气溶胶的增加相对应。我们使用 WRF-SUEWS 耦合系统,通过比较大伦敦地区人类活动的不同区域(中心商业区和住宅区),研究人为热通量排放对边界层动力学的影响--较大的人为热排放不仅会抬高混合层高度,还会导致近地面大气更加温暖干燥。
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引用次数: 0
An improved version of the piecewise parabolic method advection scheme: description and performance assessment in a bidimensional test case with stiff chemistry in toyCTM v1.0.1 改进版的片断抛物线法平流方案:在 toyCTM v1.0.1 中的二维硬化学测试案例中进行描述和性能评估
IF 5.1 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-12-22 DOI: 10.5194/gmd-16-7509-2023
S. Mailler, R. Pennel, L. Menut, A. Cholakian
Abstract. This study presents a novel method to estimate the performance of advection schemes in numerical experiments along with a semi-realistic, non-linear, stiff chemical system. This method is based on the examination of the “signature function”, an invariant of the advection equation. Apart from exposing this concept in a particular numerical test case, we show that a new numerical scheme based on a combination of the piecewise parabolic method (PPM) with the flux adjustments of Walcek outperforms both the PPM and the Walcek schemes for inert tracer advection as well as for advection of chemically active species. From a fundamental point of view, we think that our evaluation method, based on the invariance of the signature function under the effect of advection, offers a new way to evaluate objectively the performance of advection schemes in the presence of active chemistry. More immediately, we show that the new PPM + W (“piecewise parabolic method + Walcek”) advection scheme offers chemistry-transport modellers an alternative, high-performance scheme designed for Cartesian-grid Eulerian chemistry-transport models, with improved performance over the classical PPM scheme. The computational cost of PPM + W is not higher than that of PPM. With improved accuracy and controlled computational cost, this new scheme may find applications in other fields such as ocean models or atmospheric circulation models.
摘要本研究提出了一种新方法,用于在数值实验中估算平流方案的性能以及半现实、非线性、刚性化学系统的性能。该方法基于对 "特征函数 "的检验,"特征函数 "是平流方程的一个不变量。除了在一个特定的数值测试案例中揭示这一概念外,我们还表明,在惰性示踪剂平流以及化学活性物种平流方面,基于片断抛物线法(PPM)与 Walcek 通量调整相结合的新数值方案优于 PPM 和 Walcek 方案。从根本上说,我们认为我们的评估方法基于特征函数在平流作用下的不变性,为客观评估平流方案在活跃化学物质存在时的性能提供了一种新方法。更直接地说,我们证明了新的 PPM + W("piecewise parabolic method + Walcek")平流方案为化学传输建模者提供了另一种高性能方案,该方案专为笛卡尔网格欧拉化学传输模型而设计,其性能比经典的 PPM 方案有所提高。PPM + W 的计算成本并不比 PPM 高。随着精度的提高和计算成本的控制,这一新方案可能会在海洋模型或大气环流模型等其他领域得到应用。
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引用次数: 0
INCHEM-Py v1.2: a community box model for indoor air chemistry INCHEM-Py v1.2:室内空气化学群落盒模型
IF 5.1 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-12-21 DOI: 10.5194/gmd-16-7411-2023
David R Shaw, T. Carter, Helen L Davies, Ellen Harding-Smith, Elliott C. Crocker, G. Beel, Zixu Wang, N. Carslaw
Abstract. The Indoor CHEMical model in Python, INCHEM-Py, is an open-source and accessible box model for the simulation of the indoor atmosphere and is a refactor (rewrite of source code) and significant development of the INdoor Detailed Chemical Model (INDCM). INCHEM-Py creates and solves a system of coupled ordinary differential equations that include gas-phase chemistry, surface deposition, indoor–outdoor air change, indoor photolysis processes and gas-to-particle partitioning for three common terpenes. It is optimised for ease of installation and simple modification for inexperienced users, while also providing unfettered access to customise the physical and chemical processes for more advanced users. A detailed user manual is included with the model and updated with each version release. In this paper, INCHEM-Py v1.2 is introduced, and the modelled processes are described in detail, with benchmarking between simulated data and published experimental results presented, alongside discussion of the parameters and assumptions used. It is shown that INCHEM-Py achieves excellent agreement with measurements from an experimental campaign which investigate the effects of different surfaces on the concentrations of different indoor air pollutants. In addition, INCHEM-Py shows closer agreement to experimental data than INDCM. This is due to the increased functionality of INCHEM-Py to model additional processes, such as deposition-induced surface emissions. A comparative analysis with a similar zero-dimensional model, AtChem2, verifies the solution of the gas-phase chemistry. Published community use cases of INCHEM-Py are also presented to show the variety of applications for which this model is valuable to further our understanding of indoor air chemistry.
摘要Python 室内化学模型(INCHEM-Py)是一个用于模拟室内大气的开源、可访问的盒式模型,是对室内详细化学模型(INDCM)的重构(源代码重写)和重大发展。INCHEM-Py 创建并求解了一个耦合常微分方程系统,其中包括三种常见萜烯的气相化学、表面沉积、室内外空气变化、室内光解过程和气体-颗粒分配。该系统经过优化,便于没有经验的用户进行安装和简单修改,同时还为高级用户提供了不受限制的自定义物理和化学过程的权限。该模型附带有详细的用户手册,并随着每个版本的发布而更新。本文介绍了 INCHEM-Py v1.2,详细描述了建模过程,并对模拟数据和公布的实验结果进行了比对,同时讨论了所使用的参数和假设。结果表明,INCHEM-Py 与一项实验活动的测量结果非常吻合,该活动研究了不同表面对不同室内空气污染物浓度的影响。此外,与 INDCM 相比,INCHEM-Py 与实验数据的一致性更为接近。这是因为 INCHEM-Py 增加了对沉积引起的表面排放等额外过程进行建模的功能。与类似的零维模型 AtChem2 的对比分析验证了气相化学的解决方案。此外,还介绍了已发表的 INCHEM-Py 社区使用案例,以展示该模型在各种应用中的价值,从而进一步加深我们对室内空气化学的理解。
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引用次数: 0
The Framework for Assessing Changes To Sea-level (FACTS) v1.0: a platform for characterizing parametric and structural uncertainty in future global, relative, and extreme sea-level change 海平面变化评估框架 (FACTS)v1.0:描述未来全球、相对和极端海平面变化的参数和结构不确定性的平台
IF 5.1 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-12-21 DOI: 10.5194/gmd-16-7461-2023
R. Kopp, G. Garner, T. Hermans, S. Jha, Praveen Kumar, Alexander Reedy, A. Slangen, M. Turilli, T. Edwards, J. Gregory, George Koubbe, A. Levermann, André Merzky, S. Nowicki, M. Palmer, Christopher J. Smith
Abstract. Future sea-level rise projections are characterized by both quantifiable uncertainty and unquantifiable structural uncertainty. Thorough scientific assessment of sea-level rise projections requires analysis of both dimensions of uncertainty. Probabilistic sea-level rise projections evaluate the quantifiable dimension of uncertainty; comparison of alternative probabilistic methods provides an indication of structural uncertainty. Here we describe the Framework for Assessing Changes To Sea-level (FACTS), a modular platform for characterizing different probability distributions for the drivers of sea-level change and their consequences for global mean, regional, and extreme sea-level change. We demonstrate its application by generating seven alternative probability distributions under multiple emissions scenarios for both future global mean sea-level change and future relative and extreme sea-level change at New York City. These distributions, closely aligned with those presented in the Intergovernmental Panel on Climate Change Sixth Assessment Report, emphasize the role of the Antarctic and Greenland ice sheets as drivers of structural uncertainty in sea-level change projections.
摘要。未来海平面上升预测具有可量化的不确定性和不可量化的结构不确定性。要对海平面上升预测进行全面的科学评估,就必须对这两方面的不确定性进行分析。海平面上升概率预测评估的是可量化的不确定性;对其他概率方法的比较则表明了结构性的不确定性。在此,我们介绍了海平面变化评估框架(FACTS),这是一个模块化平台,用于描述海平面变化驱动因素的不同概率分布及其对全球平均、区域和极端海平面变化的影响。我们通过在多种排放情景下生成纽约市未来全球平均海平面变化以及未来相对和极端海平面变化的七种备选概率分布来演示其应用。这些分布与政府间气候变化专门委员会第六次评估报告中提出的分布密切相关,强调了南极和格陵兰冰盖作为海平面变化预测结构不确定性驱动因素的作用。
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引用次数: 9
Implementation and evaluation of updated photolysis rates in the EMEP MSC-W chemistry-transport model using Cloud-J v7.3e 使用 Cloud-J v7.3e 在 EMEP MSC-W 化学传输模式中实施和评估更新的光解率
IF 5.1 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-12-21 DOI: 10.5194/gmd-16-7433-2023
Willem E. van Caspel, David Simpson, J. Jonson, A. Benedictow, Yao Ge, A. D. Di Sarra, G. Pace, M. Vieno, Hannah L. Walker, M. Heal
Abstract. The present work describes the implementation of the state of the art Cloud-J v7.3 photolysis rate calculation code in the EMEP MSC-W chemistry-transport model. Cloud-J calculates photolysis rates and accounts for cloud and aerosol optical properties at model run time, replacing the old system based on tabulated values. The performance of Cloud-J is evaluated against aerial photolysis rate observations made over the Pacific Ocean and against surface observations from three measurement sites in Europe. Numerical experiments are performed to investigate the sensitivity of the calculated photolysis rates to the spatial and temporal model resolution, input meteorology model, simulated ozone column, and cloud effect parameterization. These experiments indicate that the calculated photolysis rates are most sensitive to the choice of input meteorology model and cloud effect parameterization while also showing that surface ozone photolysis rates can vary by up to 20 % due to daily variations in total ozone column. Further analysis investigates the impact of Cloud-J on the oxidizing capacity of the troposphere, aerosol–photolysis interactions, and surface air quality predictions. Results find that the annual mean mass-weighted tropospheric hydroxyl concentration is increased by 26 %, while the photolytic impact of aerosols is mostly limited to large tropical biomass-burning regions. Overall, Cloud-J represents a major improvement over the tabulated system, leading to improved model performance for predicting carbon monoxide and daily maximum ozone surface concentrations.
摘要本研究介绍了最先进的 Cloud-J v7.3 光解率计算代码在 EMEP MSC-W 化学传输模式中的应用。Cloud-J 计算光解率,并在模型运行时考虑云和气溶胶的光学特性,取代了基于表格值的旧系统。根据太平洋上空的航空光解率观测数据以及欧洲三个测量点的地表观测数据,对 Cloud-J 的性能进行了评估。进行了数值实验,以研究计算出的光解率对时空模型分辨率、输入气象模型、模拟臭氧柱和云效应参数化的敏感性。这些实验表明,计算出的光解率对输入气象模型和云效应参数化的选择最为敏感,同时还表明,由于总臭氧柱的日变化,地表臭氧光解率的变化可达 20%。进一步的分析研究了云-J 对对流层氧化能力、气溶胶-光解相互作用以及地表空气质量预测的影响。结果发现,对流层氢氧基的年均质量加权浓度增加了 26%,而气溶胶的光解影响主要局限于大型热带生物质燃烧地区。总体而言,Cloud-J 比表格系统有了重大改进,从而提高了预测一氧化碳和臭氧日最大表面浓度的模型性能。
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Geoscientific Model Development
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