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Here is a tentative agenda for the 2012 CMAS Conference. Each speaker is alloted 15 minutes for their oral presentation and 5 minutes for questions. We will strictly enforce these time allotments, so that we have time to accommodate everyone on the schedule. *Times listed below are subject to change.
| October 15, 2012 - Grumman Auditorium |
| 7:30 AM | Registration and Continental Breakfast |
| 8:00 AM | A/V Upload for Oral Presenters |
| 8:30 AM | Opening Remarks: Dr. Larry Band, Director, UNC Institute for the Environment |
| 8:40 AM | Keynote Address: Dr. Len Peters, Secretary of the Cabinet for Energy and Environment, Commonwealth of Kentucky |
| 9:10 AM | CMAS Update Dr. Adel Hanna, Director, CMAS |
| |
Model Development, chaired by Prakash Bhave (US EPA) and Eduardo Olaguer (Houston Advanced Research Center) |
| 9:20 AM |
Correctly representing the optical properties of black carbon in the integrated WRF-CMAQ system
Francis S. Binkowski
Institute for the Environment
The University of North Carolina At Chapel Hill
The WRF-CMAQ integrated system is designed to include the feedback effect from aerosols on the short and long wave radiation budgets. Contemporary measurements of ambient aerosol particles, especially PM2.5, indicate that these particles often consist of a Black Carbon (BC) core surrounded by a coating or shell of species such as sulfates, organics and water. Jacobson (2000) has argued that the best way of representing the absorption and scattering properties of such particles is to model them directly as a coated BC sphere. Thus, it seems very appropriate to include this coated-sphere (core-shell) approach in a new aerosol-optics package for WRF_CMAQ.
Because CMAQ produces log-normal size distributions for the aerosols, the scattering and absorption codes must be integrated over these distributions. Our computer codes use the very efficient Gauss-Hermite (GH) numerical integration method to accomplish this integration.
The integration algorithms internally call the widely accepted routines BHMIE and BHCOAT (Bohren & Huffman, 1983) to calculate the extinction and scattering efficiency coefficients as well as the asymmetry parameter. When Black Carbon is present as an aerosol species, the code automatically invokes the coated-sphere (core-shell) approach of BHCOAT. Otherwise, invoking BHMIE is the path of choice for homogeneous particles. The code also chooses an optimal set of abscissas and weights depending upon the Mie size-parameter ( pi times the geometric-mean diameter / wavelength) and the refractive index. These calculations are done for both short and long wave radiant fields.
Thus, the radiative transfer calculations in WRF-CMAQ will be more aligned with current aerosol particle observation.
Reference:
Bohren, C.F. and D.R. Huffman, 1983, Absorption and Scattering of Light by Small Particles, Wiley-Interscience , New York, copyright 1983. (Paperback published 1998).
Jacobson, M.Z., 2000, A physically-based treatment of elemental carbon optics: Implications for global direct forcing of aerosols, Geophysical Research Letters, Vol. 27, No. 2, pp 217-220, January 15, 2000
Frank Binkowski
|
| 9:40 AM |
Limei Ran
|
| 10:00 AM |
Arastoo Pour Biazar
|
| 10:20 AM |
Developing chemical mechanisms that are more robust to changes in atmospheric composition
Gookyoung Heo,a William P.L. Carter,a Greg Yarwoodb
aCollege of Engineering, Center for Environmental Research and Technology, University of California, Riverside, CA 92521, USA
bENVIRON International Corporation, 773 San Marin Drive, Suite 2115, Novato, CA 94998, USA
Chemical mechanisms commonly used for 3-dimensional air quality modeling represent the atmospheric reactions of many different volatile organic compounds (VOCs) with highly condensed reactions of a limited number of model species by using assumptions on the average air compositions of major VOC classes (e.g., alkenes) or major carbon bond types (e.g., terminal C=C bonds). These condensed chemical mechanisms are designed to model O3 formation from typical urban ambient VOC mixtures while reducing the computational burden caused by gas-phase chemistry calculations and allowing available resources to be used for improving other components of the air quality modeling (e.g., better representing emissions and meteorology). However, the atmospheric composition is not constant and changes temporally and spatially. For example, in southeast Texas, the atmospheric composition is often markedly different from that of the typical composition in most urban areas in the U.S. due to industrial emissions; the VOC composition of mobile emissions also changes as fuels and technologies change. As a result, certain compounds may warrant more attention for some regions than for other regions, and certain compounds may need more attention due to changes in emissions over time. However, using detailed mechanisms with many additional reaction parameters beyond some point where basic laboratory studies and environmental chamber studies cannot reasonably support could give us an illusion that we know better than we actually know. Furthermore, using more detailed chemical mechanisms does not guarantee significantly better model predictions (e.g., predicted O3 concentrations) than condensed chemical mechanisms while demanding more resources such as more computer memory, disk storage, and computational time. In this presentation, we will present a practical and scientifically reasonable approach to developing chemical mechanisms that are more robust to temporal and spatial changes in atmospheric composition.
Key words: chemical mechanism, condensed chemical mechanism, atmospheric composition, air quality modeling
Gookyoung Heo
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| 10:40 AM |
Break |
| 11:10 AM |
Zhen Liu
|
| 11:30 AM |
Eduardo P. Olaguer
|
| 11:50 AM |
Aika Yano
|
| 12:10 PM |
Lunch, Trillium Room |
| 1:10 PM |
Development and evaluation of plume-in-grid and volatility basis set modules in CMAQ 5.01 Prakash Karamchandani, Bonyoung Koo, Greg Yarwood, Jeremiah Johnson
ENVIRON International Corporation
Eladio Knipping
EPRI
The Community Multiscale Air Quality (CMAQ) modeling system Version 5.0 (CMAQv5.0) was released by the U.S. EPA in February 2012, and an interim release (v5.01) is currently undergoing testing before being publicly released. Because CMAQ is a community model, EPA encourages the development of proven alternative science treatments by external scientists and developers that can be incorporated as part of an official CMAQ release. This paper describes the implementation and evaluation of two new science modules for CMAQ 5.01: (1) a plume-in-grid (PinG) module, based on a reactive puff model, SCICHEM; and (2) an alternative framework for organic particulate matter (PM) formation using a volatility basis set (VBS) approach. The PinG module, also referred to as Advanced Plume Treatment (APT), provides the capability of resolving sub-grid scale processes, such as the transport and chemistry of point source plumes, in a grid model. The VBS approach provides a unified framework for gas-aerosol partitioning of both primary organic aerosols (POA) and secondary organic aerosols (SOA), including chemical aging. The VBS implementation in CMAQ 5.01 uses four separate basis sets to differentiate anthropogenic POA and SOA, biogenic SOA, and OA from biomass burning. Each basis set consists of five volatility bins including a zero-volatility bin for non-volatile compounds. Molecular weight increases as volatility decreases to account for mass gain from chemical aging. The new PinG and VBS modules in CMAQ 5.01 are applied and evaluated separately for two 15-day summer and winter periods in 2005 to the eastern U.S., and their results compared with those from the base CMAQ 5.01. Twenty large point sources of NOx in the eastern U.S. are selected for explicit plume treatment with APT in the PinG simulation. We present results from these applications of the two new modules in CMAQ 5.01.
Prakash Karamchandani
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| 1:30 PM |
Matthew Woody
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| 1:50 PM |
Havala O. T. Pye
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| 2:10 PM |
Greg Yarwood
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| 2:30 PM |
Effects of Implementing Subgrid-Scale Cloud-Radiation Interactions in WRF
Kiran Alapaty1, Jerold Herwehe1, Chris Nolte1, Russ Bullock1, Tanya Otte1, Megan Mallard1, Jimy Dudhia2, and Jack Kain3
1Atmospheric Modeling and Analysis Division, U.S. Environmental Protection Agency, Research Triangle Park, NC
2National Center for Atmospheric Research, Boulder, CO
3National Severe Storms Laboratory, National Oceanic & Atmospheric Administration, Norman, OK
Abstract: Interactions between atmospheric radiation, clouds, and aerosols are the most important processes that determine the climate and its variability, affecting air quality and environmental systems. The Weather Research & Forecasting model (WRF) is being used as a regional climate model (RCM) by many groups, including the RCM group at the EPA. One of the findings from our RCM studies is that the summertime convective systems simulated by the WRF model are highly energetic, leading to excessive surface precipitation. We also found that the WRF model does not consider the interactions between convective clouds and radiation, thereby omitting an important process that drives the climate. Thus, the subgrid-scale cloudiness associated with convective clouds (from shallow cumuli to thunderstorms) does not exist and radiation passes through the atmosphere nearly unimpeded, potentially leading to overly energetic convection. The Atmospheric Modeling and Analysis Division (AMAD) at the EPA is advancing the climate science of the cloud-aerosol-radiation (CAR) interactions by continued development of integrated modeling systems for meteorology/climate (such as WRF) and air quality (the Community Multiscale Air Quality model, CMAQ). In these models, when used at coarse spatial resolutions (e.g., larger than 1 km), convective cumulus clouds need to be modeled as subgrid-scale clouds. Thus, in order to achieve full CAR interactions of cumulus clouds with aerosols and radiation, cumulus cloud parameterizations need to be linked first with radiation processes. To this end, our research group has implemented into WRF a cloudiness formulation that is widely used in global earth system models (e.g., CESM/CAM5) to account for the effects of the cumulus clouds on radiation. Estimated grid-scale cloudiness and associated condensate are adjusted to account for the subgrid clouds and then passed to the WRF radiation schemes to affect the shortwave and longwave radiative processes. To test the implementation, two sets of WRF simulations were conducted: a one-week case study (July 24-30, 2010) to represent running WRF in numerical weather prediction (NWP) mode; and simulation of a three-year period (1988-1990) to study the effects on WRF in a regional climate mode. Results will be presented to show the effects of introducing the subgrid-scale cloud-radiation interactions on quantities such as precipitation and temperature, and the potential implications for regional air quality.
Jerold Herwehe
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| 2:50 PM |
Break |
| 3:20 - 5:30 PM | Poster Session
Air Quality Measurements and Observational Studies
Ka-Wa Chan -
Chuen-Meei Gan -
Dana M. Greene, Ph.D., M.A. -
Yukari Hara -
Recent inter-annual trend of spherical aerosol in East Asia based on integrated analysis of remote sensing and a chemical transport model
Hara, Y1., Uno, I.1, Shimizu, A.2, Sugimoto, N.2, Matsui, I.2, Itahashi, S.3 and Ohara, T.2
1 Research Institute for Applied Mechanics, Kyushu University, Kasuga, Fukuoka, Japan
2 National Institute for Environmental Studies, Tsukuba, Ibaraki, Japan.
3 Department of Earth System Science and Tecnology, Kyushu University, Fukuoka, Japan
Recent rapid economic growth of Eastern Asian countries has caused a marked increase of anthropogenic emission (Ohara et al., 2007) since 2000. However, Lu et al. (2011) reported that SO2 emission in China decreased by 9.2% from 2006 to 2010 due to the wide application of flue-gas desulfurization (FGD) devices in power plants. On the other hand, Lamsal et al. (2011) showed that NOx emission from East Asia increased by 18.8 % during 2006-2009. Anthropogenic emission in East Asia has changed dramatically by the balance between economic development and political emission control.
National Institute for Environmental Studies (NIES) has been constructing a ground-based network of automated dual-wavelength (532, 1064 nm), polarization-sensitive (532 nm) Mie-lidar systems to examine air quality continuously in eastern Asia since 2001 (Shimizu et al., 2004). In this paper, recent inter-annual trend of anthropogenic aerosols was investigated using ground-based lidar data, space-borne lidar, the Moderate resolution Imaging Spectroradiometer (MODIS) data and the Community Multi-scale Air Quality Modeling System (CMAQ) chemical transport model simulation during 2004-2011.
The increase trend of spherical aerosol optical depth (AOD) was observed over the wide region of East Asia by aerosol retrievals of lidar and MODIS from 2004 to 2008. After 2008, the decrease trend of AOD was seen in downwind region (around Japan), while increase trend of AOD was still observed in northeastern China by remote sensing. CMAQ showed that the main composition of spherical aerosol around Japan is sulfate, therefore recent AOD decrease trend in downwind region may be basically caused by the SO2 emission reduction due to the FGD devices in China. The AOD increase trend in northeastern China might be attributed by increase of secondary aerosol formed from precursor species including NOx after 2008.
Yongtao Hu -
Modeling wildfire impacts on air quality during the ARCTAS-CARB campaign: evaluation using surface, airborne and satellite measurements
Yongtao Hu1, M. Talat Odman1, Armistead G. Russell1, Xiaoyang Zhang2,3, Shobha Kondragunta3, Hongbin Yu2,4, Huisheng Bian5,4, Lorraine Remer5,
1School of Civil and Environmental Engineering, Georgia Institute of Technology, Atlanta, GA 30332
2 Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD 20740
3 NOAA/NESDIS/STAR, College Park, College Park, MD 20740
4 Earth Science Directorate, NASA Goddard Space Flight Center, Greenbelt, MD 20771
5Joint Center for Earth Systems Technology, University of Maryland at Baltimore County, Baltimore, MD 21228
Increasingly frequent wildfires in the US have led to imposed adverse impacts on rural and urban air quality. During large wildfire episodes, exceedances of NAAQS for ozone and PM2.5 are encountered. The US EPA allows these exceptional events to be exempted from being designated as exceeding NAAQS. However, how and how much the wildfires really contribute to elevated ozone and PM2.5 observations are poorly understood. The 2008 summer northern California wildfires are suspected of causing severe air pollution in the urban areas in California. With ample airborne data collected in flights chasing the fire plumes, in addition to the regular surface network measurements and satellite observations, the June-July 2008 ARCTAS-CARB campaign provides a good opportunity to evaluate the capability of regional air quality models in capturing the wildfire impacts on air quality.
We employed a state of art air quality model, CMAQ, equipped with a new SOA module including the multi-generational oxidation process to simulate the air quality impacts of the 2008 northern California wildfires. The simulation covers the period of June 15 through July 14, 2008. Three nesting grids are used with the 36-km grid covering the CONUS, the 12-km grid covering California and the 4-km grid covering most metro areas in California. All the three grids have 34 vertical layers extending to ~16km above the ground with the first layer ~18m thick. We evaluate model performance by examining ozone and PM2.5 as well as other gaseous and PM components against measurements at multi-platforms: surface, airborne and space. Further, the sensitivity analysis tool DDM-3D is used to assess the air quality impacts of fire emissions and to investigate the sources of model deficiencies regarding modeling of the fire impacts. Model bias due to uncertainties in emissions estimates, fire plume rise estimations, as well as meteorology parameters will be addressed. An inverse modeling technique will be used to quantify the uncertainties in estimates of fire emissions and in layering of those emissions vertically in the CMAQ model.
Christopher P. Loughner -
Daniel Tong -
Jonathan Trueblood -
Coupled Meteorology/Chemistry Models
Chao Wei -
Emissions Inventories, Models, and Processes
Erin Chavez-Figueroa -
Gregory Frost -
Agustín R. García -
Stephen Reid -
TL Roche -
Wei Tang -
Jia Xing -
Historical gaseous and primary aerosol emissions in the United States from 1990-2010
Jia Xing1, Jonathan Pleim1, Rohit Mathur1, George Pouliot1, Christian Hogrefe1, Chuen-Meei Gan1, Chao Wei1
1 The U.S. Environmental Protection Agency, Research Triangle Park, NC 27711, USA
It is believed that the observed evolution of decadal dimming to brightening during the 1990s in the continental United States was strongly influenced by the reductions in anthropogenic emissions of aerosol precursors. Regional chemistry or climate models are good tools for improving our understanding of the role of aerosols in the decadal changes of solar radiation. However, to perform such simulations in order to reproduce and interpret the observed phenomena, an accurate description of emission changes over such extended time periods is crucial but challenging.
In this study, we used an approach based on activity data to develop a consistent series of spatially resolved emissions in the United States from 1990 to 2010. The state-level anthropogenic emissions of SO2, NOx, CO, NMVOC, NH3, PM10 and PM2.5 for three major sectors (incl. 48 sub-sectors) were estimated based on several long-term databases containing information about changes in activity data and emission controls. Activity data for energy-related stationary sources were derived from the State Energy Data System. Corresponding emission factors reflecting implemented emission controls were calculated back from the national emission inventory (NEI) for seven years (i.e., 1990, 1995, 1996, 1999, 2001, 2002 and 2005), and constrained by the AP-42 (US EPA's Compilation of Air Pollutant Emissions Factors) dataset. Activity data for mobile sources including all types of highway vehicles and non-highway equipments was obtained from the highway statistics reported by Federal Highway Administration. The trends in emission factors for highway mobile source were informed by the 2011 National Transportation Statistics. Emissions for all non-energy related source were either scaled by the growth ratio of activity indicator or adjusted based on the NEI trends report and EDGAR (Emissions Database for Global Atmospheric Research) dataset.
Because of the strengthened control standards, particularly for the power sector and mobile sources, emissions of all pollutant except NH3 were reduced by half over the last two decades. The emission trends developed in this study are comparable with the NEI trend report and EDGAR data, but better constrained by trends in activity data. Reduction ratios in SO2 and NOx emissions agree well with the observed changes in ambient SO2 and NO2 concentrations, suggesting that the various control on SO2 and NOx emissions implemented over the last two decades are well represented in the emission inventories developed in this study. These inventories were processed by SMOKE and are now ready to be used for regional chemistry transport model simulations over the 1990-2010 period.
Global/Regional Modeling Applications
Farhan Akhtar -
Colin Cameron -
Ming Tung Chuang -
The impact of biomass burning aerosols from Southeast Asia on the West Pacific
Ming Tung Chuang1, Joshua S. Fu2, Fang-Yi Cheng3, Neng-Huei Lin3, Chung-Te Lee1
1. Graduate Institute of Energy Engineering & Sustainable Environmental Technology Research Center, National Central University, Jhung-Li, Taoyuan 32001, Taiwan
2. Department of Civil and Environmental Engineering, University of Tennessee, Knoxville, Tennessee, USA
3. Department of Atmospheric Sciences, National Central University, Jhung-Li, Taoyuan 32001, Taiwan
As for the influence of biomass burning aerosols from Indochina on Taiwan and neighborhood area during long-range transport, certain understanding of aerosol properties has been obtained through years of observation experiments. However, all these experiments can only tell us the information of aerosols at Mt. Lulin Mountains in Central Taiwan when air masses were from Indochina or southern China. The characteristics of aerosol components analyzed at the receptor cannot tell us the evolution of chemical species during long-range transport and the radiative effects over Taiwan and neighborhood.
This study will apply CMAQ model to simulate aerosol chemistry along the path of long-range transport from Southeast Asia to Taiwan. The meteorology input was from WRF model. The emissions of anthropogenic sources, biogenic sources, and biomass burning emissions were processed into hourly resolution, respectively. The simulation results were validated by observations from other sub-projects which analyzed chemical components of aerosols collected at Mt. Lulin and regional observation in South China Sea. It is found that even the simulation uncertainty has reduced the precision of comparison between the simulated and the measured concentration, this preliminary study still reveals the chemical evolution of biomass burning aerosols and precursors in the biomass burning plume from Indochina, and influence of aerosols on radiative effects around Taiwan.
Kenneth Craig -
Agustín R. García -
Coupled Meteorology-Chemistry Model Application for Evaluation of Climate Change Influence on Air Quality: Central Mexico Case Study.
Agustín R. García1, Aidee Vega-Rodriguez1, Ernesto Caetano2, Daniela Cruz-Pastrana1, Manuel Suarez-Lastra2
Universidad Nacional Autónoma de México
1Centro de Ciencias de la Atmósfera
2Instituto de Geografía
Meteorology can impact the ambient concentrations of pollutants; warmer weather can enhance atmospheric reactivity but also can influence atmospheric dynamic processes. With a coupled model both effects can be taken into account. In order to evaluate the impact of climate change on air quality, a coupled meteorology chemistry model is applied for central Mexico for two different climate scenarios, (base case and A1B for 2070).
Meteorological data using a dynamic downscaling from climate scenario is used in order to obtain the initial and boundary conditions for base case 1980 and 2070 decades. The radiation module used considers modifications in gas trace compounds. In order to identify the influence of climate two different scenarios were considered a) using base case emissions and 1980 meteorological conditions, b) using base case emissions and 2070 meteorological conditions. Emissions projection was based only in the urban sprawl projection. Case a) and b) were used for identify only the climate influence in the air quality in the region.
The WRF-chem model incorporates chemical transformations and complex gas-phase chemistry, photolysis and aerosols interactions, and is applied using different meteorological senarios.
To evaluate the effect of ozone concentrations in the population, three metrics from Georgopoulos et al. 1997 were used: severity, pervasiveness and potential integrated exposure. Severity sums the times that a concentration exceeds a threshold level (110ppb for ozone). Pervasiveness is the sum of grid cells that registered concentrations above the threshold level during the evaluation period, and the integrated potential exposure measures the exposure in time and space, considering the number of population potentially exposed to outdoor hazardous levels. Results from the base scenario 1980 and 2070 climate scenario.
Results show an increase in temperature in the region; in some periods the mixing height layer increased inducing a decrement of pollutants, like ozone and aerosols, concentrations.
Yoo Jung Kim -
Peng Liu -
Megan Mallard -
Raquel Silva -
Nicholas Witcraft -
Yu-Han Cheng -
Steve H.L. Yim -
Yuqiang Zhang -
Effects of changes in emissions and climate change on global air quality: a study of the air quality co-benefits of GHGs mitigation
Yuqiang Zhang1, J. Jason West1, Meridith Fry1, Zac Adelman1, Raquel Silva1, Steve Smith2, Vaishali Naik3, Susan Anenberg4, Larry W. Horowitz5, Jean-Francois Lamarque6
1The University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 27599
2Joint Global Change Research Institute, Pacific Northwest National Laboratory, 5825 University Research Court, Suite 3500, College Park, MD 20740, USA
3Atmospheric Physics, Chemistry, and Climate Group, UCAR GFDL, Princeton, New Jersey, USA
4U.S. Environmental Protection Agency, Washington, DC, USA
5Geophysical Fluid Dynamics Laboratory, National Oceanic and Atmospheric Administration, 201 Forrestal Road, Princeton, NJ 08540, USA
6Atmospheric Chemistry and Climate and Global Dynamics Divisions, National Center for Atmospheric Research, Boulder, CO 80307, USA
Air quality can be affected by both pollutant emissions and meteorological conditions which influence the transport and chemical transformation processes. Actions to mitigate Greenhouse Gases (GHGs) emissions therefore will yield air quality co-benefits from two mechanisms in the future: one directly through the reductions in the emissions of co-emitted air pollutants (short-term and local); another indirectly from slowing the influence of climate change on air pollution (long-term and global). We have completed simulations using the MOZART-4 global chemical transport model that are designed to quantify the co-benefits of GHG mitigation by these two mechanisms in future years. Here we aim to explain the changes in ozone and fine particular mater (PM2.5) that we modeled, in terms of changes in emissions and meteorological variables due to climate change. We emphasize the different factors controlling the air quality co-benefits by these two mechanisms, including changes in co-emitted air pollutants, biogenic emissions variations, soil NOx emissions, and other meteorological factors such as water vapor, temperature, and surface solar radiation, and analyze the influence of these factors in contributing to the change of ozone and PM2.5. We will present results for the changes in global air quality due to GHG mitigation in 2030, 2050, and 2100. For this study, future emission scenarios were developed by the GCAM global energy-economics model as part of the Representative Concentration Pathways (RCP) process, where we focus on the RCP4.5 scenario, and the GCAM reference emission scenario. Future meteorological conditions are from general circulation model simulations of RCP4.5 and RCP8.5 from the Geophysical Fluid Dynamics Laboratory (GFDL). By analyzing combinations of emissions and meteorology from different scenarios, we isolate the co-benefits of GHG mitigation from reductions in co-emitted species and from those due to slowing down climate change.
Model Development
Fernando Garcia-Menendez -
Ketsiri Leelasakultum -
Golam Sarwar -
Zhining Tao -
Daniel Tong or George Bowker -
Recent updates in the CMAQ windblown dust emission module
Daniel Tong1,2, George Bowker3, Fantine Ngan4, George Pouliot5, Pius Lee4
1 NASA GES/DISC, NASA Goddard Space Flight Center, Greenbelt, MD
2 CSISS, George Mason University, Fairfax, VA
3 US Environmental Protection Agency, Clean Air Markets Division, Washington, DC
4 NOAA Air Resources Laboratory, Silver Spring, MD
5 US EPA Atmospheric Modeling and Analysis Division/NERL/ORD, RTP, NC
Dust emitted during windstorms is an important component of the atmosphere, affecting climate as well as air quality. Previously, we have created a windblown dust emission module for use within CMAQ. Here, we present three potential improvements to this module: chemical composition profile, soil moisture effect, and wind bias adjustment. Currently, the chemical profile of CMAQ windblown dust is based on anthropogenic dust composition, which may not be consistent with natural dust particles originating from deserts and semi-arid regions. We have developed a new approach to identify local dust events from the IMPROVE routine aerosol monitoring network, and reconstructed a database of dust events for the western United States. An updated chemical profile for natural dust particles is compiled through the analysis of the speciated aerosol data from these identified dust events and through the comparison of the US dust profile to previously reported profiles from elsewhere. We have also updated the soil moisture treatment in the dust module, as the previous codes did not consider variations in the units of soil moisture data provided by different meteorology models. Finally, we present the impact of wind bias on dust emission estimates, and propose an adjustment measure to improve dust modeling.
Model Evaluation and Analysis
Taciana Albuquerque -
K. Wyat Appel -
Examining the performance of trace metals estimates in CMAQv5.0 K. Wyat Appel, Heather Simon, George Pouliot, Havala Pye, Sergey Napelenok, Farhan Akhtar and Shawn J. Roselle
The latest version of the Community Multiscale Air Quality Model (version 5.0) includes explicit tracking and treatment of trace metals (i.e. Fe, Ca, Mg, Mn, K, Si, Al, Ti), which in previous versions of the model were treated as a single soil species. The explicit treatment of trace metals is important, as they can make up a sizeable fraction of the total fine particulate matter (dependent on location and time of year) and can also affect the model chemistry. There are both natural (e.g. dust) and anthropogenic (e.g. coal combustion) sources of trace metals, and as such the model performance for these elements is particularly sensitive to the specification of both the emissions inputs and boundary conditions. The latest version of the CMAQ model contains an updated treatment for wind-blown dust and updates to the anthropogenic fugitive dust estimates, both of which have a large impact on the model estimates of trace metals. The CMAQv5.0 model has been used to simulate the entire year of 2006, and the model estimates of the trace metals has been compared to observations from the CSN and IMPROVE networks. The results of this evaluation will be presented, along with results from several model sensitivity simulations highlighting the impact that the wind-blown dust treatment and anthropogenic fugitive dust updates have on the model estimates.
George Delic -
Kristen Foley -
Agustín R. García -
J. Godowitch -
Ikeda Kohei -
James Kelly -
Chris Misenis -
David-anthony Murray -
Li Pan -
Qi Fan -
Process analysis of PM concentration over Pearl River Delta region, China using MM5-CMAQ model
Qi Fan1, Wei Yu1, Shaojia Fan1, Jing Lan1, Yerong Feng2
1 Department of Atmospheric Sciences, Sun yat-sen University, Guangzhou, 510275, China
2 Guangzhou Central Meteorological Observatory, Guangzhou, 510080, China
As one of the three large economic regions of China, the regional air pollution, in which the primary is aerosol pollution, is serious over the Pearl River Delta (PRD) region. The main synoptic systems influencing the air quality include the Stationary Front, the Warm High, the Tropical Cyclone and so on. This study focuses on the influences of the warm high on the aerosol pollutions, with the simulations by Models-3/CMAQ system and the observations from China “973” national projects in 2004.
The results show the spatial distributions of air pollutants are circular around Guangzhou and Foshan cities with high emissions. The primary pollutant is particulate matter over the PRD. The pollution range of NOX is bigger than that of SO2, though with lower concentrations. Both MM5 and CMAQ show reasonable performance for major meteorological variables (i.e., temperature, relative humidity, wind direction, planetary boundary layer height) with normalized mean biases (NMBs) of 4.5–38.8%. The temporal variations of surface concentrations SO2, NO2, O3 and PM2.5 were captured well by CMAQ model. Relatively poor performance was found in the simulated maximum concentrations of all pollutants, the CMAQ systematically underpredicted the mass concentrations.
The process analysis (PA) results show that the emission, dry deposition, horizontal transport and vertical transport are four main processes to air pollutants. The contributions of horizontal and vertical transport processes were different during the period, but in all, these two processes contributed to the removal of air pollutants. Besides, the contributions of the same physical process were different for various pollutants, the dry deposition was vital to the removal of PM10. NOx was affected by the transport process obviously. For this high pressure case, the contributions of various processes show higher correlations in the cities with similar geographical environment. According to the statistic results, the cities in PRD region can be divided into four types with different features.
Charles Stanier -
Yadong Xu -
Xin Zhang -
Modeling Secondary Impacts from Single Sources or Single Source Complexes
Charles Chemel -
Source-Receptor Modeling and Analysis
Sivaraman Balachandran -
Kenneth Craig -
Xinyi Dong -
Assessment of air quality response to anthropogenic emission changes over Taiwan using response surface modeling methodXinyi Dong1, Joshua S. Fu1, Carey Jang2, and Hsin-Chih Lai3, and Ciao-Kai Liang4
1Department of Civil and Environmental Engineering, The University of Tennessee, Knoxville, TN
2Office of Air Quality Planning and Standards, USEPA, Research Triangle Park, NC
3Chang Jung Christian University, Environmental Research and Information Center,
Taipei, Taiwan
4Department of Air Pollution Control, Taiwan EPA, Taipei, Taiwan
Air quality is usually strong correlated with local anthropogenic emissions. A number of studies have been conducted with air quality models for Europe and United States: Tsimpidi et al. (2007) applied a three-dimensional chemical transport model (PMCAMx) for in January and July 2002 to examine the NH3 emission impact on inorganic aerosol; Pinder et al. (2007) applied the same model for July 2001 and January 2002 and reported that NH3 control in winter is more cost-effective to reduce PM2.5 than controlling NOx and SO2; Derwent et al. (2009) reported the nonlinear mass concentrations of PM with precursor emission in UK based on air parcel trajectory. While these studies were targeted to examine impacts of NH3 on total PM2.5 over populated area, knowledge of impacts of anthropogenic emission on ozone and aerosol formation in Taiwan, which is one of the most populated area, is still very limited. In addition, the remaining uncertainties, such as the nonlinearity and seasonality of ozone and aerosol responses, from different emission sectors remain unknown from the published studies.
Therefore, in this study the integrated MM5/CMAQ modeling system is applied over Taiwan to examine the O3 and PM2.5 response to ammonia emission changes using Response Surface Modeling (RSM) method. RSM has been successfully applied in China to predict O3 and PM2.5 response under sector-dependent emission control (Xing et al., 2011; Wang et al., 2011). In this study, seasonality of inorganic PM2.5 response is also investigated with four different months (January, April, July, and October) as representatives for different seasons in 2007. Impacts of ammonia emission from four different sub-areas in Taiwan is also identified and analyzed to quantify the inter-state transport impacts on inorganic PM2.5 formation over Taiwan.
Reference:
Pinder, R. W.; Adams, P. J.; Pandis, S. N. Ammonia Emission Controls as a Cost-Effective Strategy for Reducing Atmospheric Particulate Matter in the Eastern United States. Environ. Sci. Technol. 2007, 41, 380386.
Tsimpidi, A. P.; Karydis, V. A.; Pandis, S. N. Response of Inorganic Fine Particulate Matter to Emission Changes of Sulfur Dioxide and Ammonia: The Eastern United States as a Case Study. J. Air Waste Manage. Assoc. 2007, 57, 14891498, DOI: 10.3155/1047-3289.57.12.1489.
Wang, S.X.; Xinag, J.; Zhu, Y.; Fu, J.S.; Hao, J.M. Impact assessment of ammonia emissions on inorganic aerosols in east China using response surface modeling technique. Environ. Sci. Technol. 2011, 45, 9293-9300.
Xing, J.; Wang, S. X.; Chatani, S.; Zhang, C. Y.; Wei, W.;Klimont, Z.; Cofala, J.; Amann, M.; Hao, J. M. Projections of Air Pollutant Emissions and its Impacts on Regional Air Quality in China in 2020. Atmos. Chem. Phys. 2011, 11, 31193136, DOI: 10.5194/acp-11-3119-2011.
Dongwei Wu -
Chris Emery -
Kristen Foley -
Meridith M. Fry -
Global net radiative forcing responses to regional CO and NMVOC reductions
Meridith M. Fry1, M. Daniel Schwarzkopf2, Zachariah Adelman1, J. Jason West1
1Department of Environmental Sciences and Engineering, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina, USA.
2 Atmospheric Physics, Chemistry, and Climate Group, NOAA GFDL, Princeton, New Jersey, USA.
We analyze the global annual net radiative forcing (RF) impacts of regional reductions in anthropogenic carbon monoxide (CO) and non-methane volatile organic compound (NMVOC) emissions due to changes in the tropospheric concentrations of ozone (O3), methane (CH4), and aerosols. We present the RF responses to CO and NMVOC emission reductions from 10 regions (North America, South America, Europe, Former Soviet Union, Southern Africa, India, East Asia, Southeast Asia, Australia and New Zealand, and Middle East and Northern Africa). The global chemical transport model MOZART-4 is used to simulate the tropospheric concentration changes, using the IPCC AR5 Representative Concentration Pathway 8.5 (RCP 8.5) emissions inventory for 2005 and global meteorology from the Goddard Earth Observing System Model, version 5 (GEOS-5) for the years 2004-2005. We utilize the NOAA Geophysical Fluid Dynamics Laboratory standalone radiative transfer model to calculate the stratospheric-adjusted net RF for each regional CO and NMVOC reduction, relative to the base. We present estimates of the global annual net RF and the RF by latitude band (90oS – 28oS, 28oS – 28oN, 28oN – 60oN, and 60oN – 90oN). The net RF distributions for the CO and NMVOC reductions show widespread cooling across the northern and southern hemispheres corresponding to the patterns of O3 and CH4 decreases, and localized positive and negative net RFs due to increases and decreases in aerosols. The strongest annual net RF impacts occur within the tropics (28oS – 28oN) followed by the northern mid-latitudes (28oN – 60oN), for all CO emissions reductions and many of the NMVOC reductions. These estimates of RF by world region are intended to inform coordinated actions addressing air quality and climate forcing.
Amir Hakami -
Heather A. Holmes -
Development of a Mixtures Characterization Toolkit: Estimating air pollution source impacts to investigate air quality and human health associations using time-series epidemiologic analysis
Heather A. Holmes1, Marissa L. Maier1, Mariel Friberg1, Sivaraman Balachandran1, Cesunica Ivey1, Yongtao Hu1, Armistead G. Russell1, James A. Mulholland1, Stefanie E. Sarnat2, Jeremy A. Sarnat2, Matthew J. Strickland2, Andrea Winquist2, Mitchel Klein2, Paige E. Tolbert2
1Georgia Institute of Technology, Atlanta, GA, USA 2Emory University, Atlanta, GA, USA
Air pollution concentrations measured from regulatory monitoring networks are commonly used as air quality metrics in time-series epidemiologic analysis to investigate air quality and human health associations. While these data provide useful indicators for air pollution impacts in a region, the data are limited temporally, spatially and chemically. Additionally, the species concentrations cannot directly identify the emission sources or characterize the pollutant mixtures. These data in combination with chemical transport models (CTM) and source apportionment (SA) techniques can be used to characterize pollutant mixtures, sources and species impacting both individual locations and wider areas. Extensive analysis using a combination of these approaches may be beneficial for health studies whose goal is to assess the health impacts of pollutant mixtures. As part of the EPA-funded Southeastern Center for Air Pollution and Epidemiology (SCAPE), a Mixtures Characterization (MC) Toolkit is being developed to effectively analyze air pollution and air quality modeling data to better understand and quantify how emission sources combine to impact air quality and to provide metrics for use in health assessments.
Statistical data analysis is done using the species concentrations to calculate a time-series of spatial air pollution metrics based on both area and population weighted averages. Source impacts are estimated using receptor oriented SA methods (CMB, PMF, integrated indicators) and source oriented modeling from a CTM. The CTM used in this work is CMAQ, which uses emissions modeling (SMOKE) to generate a spatial and temporal allocation of the source emissions. The MC Toolkit incorporates two novel SA techniques, the first an ensemble method that generates new source profiles for CMB based on an ensemble-trained approach utilizing SA results from CMB, PMF and CMAQ. The second is a hybrid source-receptor model approach that adjusts the CMAQ source impacts based on a scaling factor obtained using CMAQ simulations and observations in a CMB-approach. In addition to source characterization, exposure estimates are a knowledge gap in health studies, thus another objective of the MC Toolkit is to develop spatial averaging and temporal interpolation components to improve the concentration distribution modeling for species concentrations and source impact estimates.
This work will present results using the MC Toolkit for two regions with differing source emissions, St. Louis, Missouri and Atlanta, Georgia. There is a significant impact of point source emissions, e.g., chemicals manufacturing and metals processing, on the air pollution in St. Louis. While in Atlanta large biogenic emissions interact with emissions from mobile sources and power plants which lead to a large amount of secondary organic aerosol formation. In the future, the MC Toolkit will be used with observations from regulatory and specialty monitoring networks to investigate the extent of city-to-city variability in pollutant mixtures and associations with health outcomes.
*This research was supported, in part, by USEPA grant R834799. Its contents are solely
the responsibility of the grantee and do not necessarily represent the official views of the
USEPA. Further, USEPA does not endorse the purchase of any commercial products or
services mentioned in the publication. Additional support was made possible by grants from Georgia Power and the Southern Company.
Xiangting Hou -
Cesunica Ivey -
Extending the Hybrid Source Apportionment Method by Spatial Interpolation of Source Impact Adjustment Factors
Cesunica Ivey1, Heather Holmes1, Yongtao Hu1, Armistead G. Russell1, and James A. Mulholland1
1Georgia Institute of Technology, Atlanta, GA
Data from air quality studies are increasingly used in health studies to assess associations between ambient concentrations of air pollutants and health. Of interest are the sources of pollutants and the magnitude of the impact that the sources have on ambient concentrations. Source impacts cannot be directly measured, leading to the application of source apportionment methods to measurable air quality indicators (e.g. daily pollutant concentrations, daily emissions from regulated sources, species profiles of emission plumes) to determine source impacts. Current source apportionment methods are derived from receptor modeling (RM) or chemical transport modeling (CTM) techniques. Both techniques present inherent challenges and uncertainties including the absence of physical and chemical processes in RM and the exclusion of monitor data in CTM, in most cases.
A hybrid source apportionment method was developed that utilizes aspects of both RMs and CTMs to integrate physical and chemical processes, observation data, as well as uncertainty estimates for model inputs. Previously, this hybrid method was applied to Chemical Speciation Network (CSN) data to determine source impacts at receptors for reporting days in January 2004. Here, the hybrid method was extended to perform source apportionment for the contiguous U.S. by spatial kriging of source impact adjustment factors, which modify original source impact simulations to reflect observed concentrations. These factors were applied to the original source impact estimates to reconstruct species concentrations for PM2.5, EC, SO42-, K, Fe, Se, and Si at Interagency Monitoring for the Protection of Visual Environments (IMPROVE) monitor locations.
Species reconstruction at IMPROVE locations was employed to assess the performance of the hybrid-kriging (HK) method at locations beyond the CSN receptor locations. On average, HK reconstructed concentrations were closer to observations than original CMAQ simulations. The average concentrations of PM2.5 for reporting days in January 2004 were 6.15 ± 1.47, 11.08 ± 3.75, and 9.28 ± 2.70 µg/m3 for observations, CMAQ, and HK simulations, respectively. Trends were similar for all other species, with the exception of Se. Both methods under-simulated Se concentrations, but CMAQ simulations were closer to observations. CMAQ and HK concentrations were biased high for all species except Se, and for all other metal species the simulated concentrations were significantly higher than observations. For nonmetal species and total PM, 60.4 ± 11.9% of CMAQ simulations and 68.8 ± 14.2% of HK simulations were within a factor of two of observations. For metal species, 30.6 ± 14.4% of CMAQ simulations and 35.0± 12.5% of HK simulations were within a factor of two of observations. Overall, the HK method is useful for performing source apportionment over large domains with enhanced spatial resolution, taking into account observed data, emissions, meteorology, and terrain.
Jong-Jae, Lee -
Simulation of source-receptor relationships for ozone in South Korea
Jong-Jae, Lee, Cheol-Hee, Kim
The rapid growth in many Asian economies in recent years has resulted in degradation of air quality in the region. In particular, ozone and aerosol aggravates respiratory illness and may lead to premature mortality [World Health Organization, 2005]. Tropospheric ozone is produced via the photochemical oxidation of volatile organic compounds (VOC) and carbon monoxide (CO) in the presence of nitrogen oxides (NOx). However some precursors (or ozone) are transported from source regions to receptor regions. In this study, source-receptor relationships of ozone are simulated in South Korea, and the impact of long-range transport on ozone concentrations are interpreted through the simulations of source-receptor relationships.
During study periods (April and July, 2009), the weather conditions of East Asia were simulated with ARW-WRF version 3.2 at 60 km horizontal grid resolution with 23 vertical layers. The NCEP FNL data was used as initial and boundary conditions for the simulations. For air quality simulations, the Community Multiscale Air Quality (CMAQ) model version 4.7 was used with a domain targeting the East Asia. Source-receptor relationships are quantified using the Brute Force method as emission changes (25% reduction of NOx and VOC) over source regions (3 parts of China, South Korea and Japan).
We calculate the spatial average surface ozone concentration over each of the five regions by carrying out six simulations including base case and five cases of emission reductions in 3 regions of China (Northern, Central, and Southern China), Japan, and South Korea. In the base simulation, spatial mean surface ozone concentrations are found to be similar: 42.1 ppb for North China, 51.1 ppb Middle China, 45.3 ppb South China, 41.9 ppb for South Korea and 33 ppb for Japan in July. The simulation generally captures the observed daily cycle and is simulated to be close to the observed ozone concentration in Seoul in South Korea.
Reduction of emissions in the three Chinese regions simulated a decreased spatial mean concentration of 3.1 ppb over South Korea especially in April, showing much lower than that of case of the emission reduction in South Korean which is 4.3 ppb. The response of South Korean surface ozone concentrations to Chinese emissions is much larger in April due to relatively lower precipitation than that in other months such as in July. High ozone concentrations in April in South Korea are relatively much more sensitive to foreign emissions than other months, as indicated by the foreign (Chinese) emission reduction cases of 13.8 ppb with the daily maximum 8-h average ozone concentrations above 60 ppb. In July, however, domestic (i.e., over the source region itself) sensitivity is larger (19.1 ppb) than foreign sensitivity (10.7 ppb).
Sensitivity of boundary conditions to source receptor relationships show higher in April than other months. Our study shows, for example in April, boundary condition contributed to Seoul concentrations about 65 % in April but it shows much lower value of about 30% in July over South Korea.
Charles Stanier -
The Adjoint of the CMAQ Aqueous Chemistry Module
JAEMEEN BAEK (1), Stanier, C. O. (1), Saide, P. E. (1), Carmichael, G. R. (1); Henze, D. (2); Turner, M.(2); Zhao, S. (3); Hakami, A.(3); Resler, J.(4); Sandu, A. (5); Russell, A. (6); Jeong, G. (2); Nenes, A. (6); Capps, S.(6); Percell, P. B. (7); Pinder, R. (8); Napelenok, S.(8); Bash, J. (8); Chai, T. (9); Byun, D. (9)
(1) University of Iowa; (2) University of Colorado at Boulder; (3) Carleton University; (4) ICS Prague; (5) Virginia Tech; (6) Georgia Tech; (7) University of Houston; (8) US EPA; (9) NOAA
In the presence of clouds, gas and aerosol phase species can dissolve into water droplets and participate in aqueous phase chemical reactions, changing the concentrations of those species significantly. These important processes oxidize S(IV) to S(VI), convert gaseous species to aerosol phase species, and remove both aerosol and gas phase components via deposition. The Community Multiscale Air Quality (CMAQ) model simulates aqueous chemistry as a part of cloud dynamics. The aqueous chemistry module includes wet deposition, scavenging, gas-aqueous phase partitioning, dissociation, formation of secondary organic aerosol and aqueous phase oxidation reactions that form sulfate and secondary organic aerosol. As part of a broader effort to develop adjoint applications of CMAQ for aerosol (CMAQ-ADJ) such as data assimilation and receptor-based sensitivity calculations, our objective is to create the adjoint model for the aqueous chemistry processes. CMAQ aqueous chemistry is implemented using the Kinetic PreProcessor (KPP), which allows for easier updating of mechanisms, and automated generation of the adjoint model. We discuss the pros and cons of the new KPP-based forward model for aqueous chemistry, and intercompare calculated sensitivities between the forward model (finite differences) and the adjoint sensitivities within both a box model and CMAQ.
Matthew Turner -
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| October 16, 2012 |
| | Grumman Auditorium |
Dogwood Room |
| 7:30 AM | Registration and Continental Breakfast |
| 8:00 AM | A/V Upload for Oral Presenters | A/V Upload for Oral Presenters |
| |
Model Evaluation and Analysis, chaired by Talat Odman (Georgia Tech) and James Boylan (Georgia Department of Natural Resources) |
Emissions Inventories, Models, and Processes, chaired by Joseph Vaughan (Washington State University) and Rich Mason (US EPA) |
| 8:30 AM |
Sharon Phillips
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Prakash Bhave
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| 8:50 AM |
Comparing differences in model performance between the coupled and non-coupled versions of WRF-CMAQv5.0 K. Wyat Appel, Shawn J. Roselle and David C. Wong
The U.S EPA recently released version 5.0 of the Community Multiscale Air Quality (CMAQ) model. The latest version of the model includes the ability to run the model in coupled mode, meaning that the meteorological driver (WRF) and chemical transport model (CTM) are run in conjunction with each other, as opposed to the non-coupled version of the model in which the meteorological driver is run first, and then used to drive the CTM. The advantage of the coupled WRF-CMAQ simulation is that it allows for feedback to occur between the meteorological and chemical fields within WRF and CMAQ. These feedbacks can result, for example, in changes in radiation and cloud formation within WRF and CMAQ, which cannot be accounted for in the non-coupled version of the model. This work will examine the difference in model performance between a coupled WRF-CMAQ simulation and non-coupled WRF-CMAQ simulation covering the entire year of 2006. Differences in meteorological and chemical fields will be examined to assess the impact that coupling the meteorological and chemical models have on the model estimates. Both model-to-model and model-to-observation comparisons will be made.
K. Wyat Appel
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BH Baek
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| 9:10 AM |
Christian Hogrefe
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Caroline M. Farkas
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| 9:30 AM |
Sensitivity analysis of influencing factors on PM2.5 nitrate simulation
Hikari Shimadera1, Hiroshi Hayami1, Satoru Chatani2, Yu Morino3, Yasuaki Mori4, Tazuko Morikawa5, Kazuyo Yamaji6, Toshimasa Ohara3
1Central Research Institute of Electric Power Industry, Abiko, Japan
2Toyota Central R&D Labs., Inc., Nagakute, Japan
3National Institute for Environmental Studies, Tsukuba, Japan
4Japan Weather Association, Tokyo, Japan
5Japan Automobile Research Institute, Tsukuba, Japan
6Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan
Fine particulate matter (PM2.5) has been of increasing concern because it may seriously affect human health. The air quality standard for PM2.5 is not attained in most urban areas in Japan. Although air quality models with reasonable accuracy are essential tools to develop and evaluate measures to attain the standard, current air quality models cannot adequately simulate atmospheric mass concentrations of PM2.5 and its components. In this study, the Community Multiscale Air Quality modeling system (CMAQ) was applied to the Kanto region of Japan in winter 2010 and summer 2011. Comparisons of the model results with PM2.5 observations indicated that CMAQ overestimated PM2.5 NO3- concentration. Sensitivity analysis was conducted in order to investigate factors influencing the model performance for PM2.5 NO3- simulation. The sensitivity analysis included following factors: variations of air temperature (-5 to +5 K), variations of NOX emission (-40 to +40 %), modification of seasonal variation of NH3 emission, parameterizations of N2O5 heterogeneous reaction probability, and variations of gaseous HNO3 and NH3 dry deposition velocities (0.2 to 5 times). These analyses indicated considerable sensitivity of air temperature, NH3 emission and dry deposition velocity to PM2.5 NO3- concentration. While current meteorological models well simulate air temperature, there are large uncertainties in estimates of NH3 emission and dry deposition velocity. Therefore these two are key factors to improve the model performance for PM2.5 NO3- simulation.
Hikari Shimadera
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Rich Mason
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| 9:50 AM |
Ivanka Stajner
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Alexis Zubrow
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| 10:10 AM |
Break |
Break |
| 10:40 AM |
María-Teresa Pay
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Yunsoo Choi
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| 11:00 AM |
Morgan L. Silverman
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Junhua Zhang
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| 11:20 AM |
Greg Yarwood
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George Pouliot
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| 11:40 AM |
Diagnostic Evaluation of a Modeling System for Predicting the Air Quality Impacts of Prescribed Burns
M. Talat Odman, Fernando Garcia-Menendez, Aika Yano and Yongtao Hu
School of Civil and Environmental Engineering, Georgia Institute of Technology, Atlanta, GA, 30332-0512, USA
Gary L. Achtemeier, Yongqiang Liu and Scott L. Goodrick
Center for Forest Disturbance Science, USDA Forest Service, Athens, GA, 30602-2044, USA
Roby Greenwald
Rollins School of Public Health, Emory University, Atlanta, GA, 30322, USA
Brian Gullett, Johanna Aurell, and William R. Stevens
Office of Research and Development, US Environmental Protection Agency, Research Triangle Park, NC, 27711, USA
Roger D. Ottmar
Pacific Northwest Research Station, Pacific Wildland Fire Sciences Laboratory, USDA Forest Service, Seattle, WA, 98103, USA
Robert J. Yokelson and Sheryl K. Akagi
Department of Chemistry, University of Montana, Missoula, MT, 59812, USA
|
A modeling system has been developed with the purpose of predicting the downwind air quality impacts of prescribed burns. The system incorporated several new elements into emission, dispersion and transport process components, all with significant potential for improving the accuracy of the predictions. Components of the modeling system were evaluated individually and together using field data from monitored burns and observations from regional networks and satellites. Field data include measurements of: 1) fuels before and after the burns, 2) emissions with an aerostat, 3) winds with ground-based and airborne instruments, 4) plume height with a lidar ceilometer, 5) short-range smoke with ground-based stationary and mobile platforms, and 6) long-range smoke with aircraft. Modeling results were compared to other models. Uncertainties in the estimation of emissions and prediction of winds were identified and quantified. Sensitivities of predicted downwind smoke concentrations to emission strength and timing, plume injection height versus PBL height, and wind speed and direction were calculated.
The objective of this presentation is to synthesize the results of component and system evaluations, uncertainty estimations and sensitivity analyses to determine where future research would be most beneficial for increasing the accuracy of the modeling system. Lessons learned will be pieced together towards a general approach for diagnostic evaluation of complex modeling systems.
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M. Talat Odman
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S. Napelenok
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| 12:00 PM |
Lunch, Trillium Room |
Lunch, Trillium Room |
| |
Model Evaluation and Analysis, continued |
Modeling Secondary Impacts from Single Sources or Single Source Complexes, chaired by Kirk Baker (US EPA) |
| 1:00 PM |
Modeling impact of biomass burning on air quality in Southeast and East Asia
Kan Huang a, Joshua S. Fu a,b,*, N. Christina Hsu c, Yang Gao a, Xinyi Dong a, Si-Chee Tsay c, Yun Fat Lam a
a Department of Civil and Environmental Engineering, The University of Tennessee, Knoxville, Tennessee, USA
b UTK-ORNL Center for Interdisciplinary Research and Graduate Education, Knoxville, Tennessee, USA
c Goddard Space Flight Center, NASA, Greenbelt, Maryland, USA
A synergy of numerical simulation, ground-based measurement and satellite observation was applied to evaluate the impact of biomass burning originating from Southeast Asia (SE Asia) within the framework of NASAs 2006 Biomass-burning Aerosols in South-East Asia: Smoke Impact Assessment (BASE-ASIA). Biomass burning emissions in the spring of 2006 peaked in March - April when most intense biomass burning occurred in Myanmar, northern Thailand, Laos, and parts of Vietnam and Cambodia. CMAQ could reasonably well simulate the spatial pattern and temporal variations of CO in comparison to both satellite and ground measurement. Overestimation or underestimation occurred in different regions due to great uncertainties of the biomass burning emission inventory. The largest discrepancy between modeled and observed CO occurred in northern Thailand, which overestimated the peak episodes by a factor of 2 - 3. In the other regions of Thailand where less fires occurred, the simulation performed much better. Scenario simulation not only modeled significant impact of biomass burning on AOD (0.4 - 0.6) in SE Asia source regions, but also in the downwind regions. The Asian spring monsoon facilitated the impact of biomass burning extending from peninsular SE Asia to the South China Sea, the Taiwan Strait, and some provinces in southern China. Different spatial distribution patterns of biomass burning AOD between March and April were caused by the different wind fields. Evaluation of several datasets, i.e, EANET, AERONET, and Taiwan supersites data, illustrated distinct regional differences of aerosol chemical and optical properties. Local biomass burning, anthropogenic sources and long-range/regional transport were the main factors controlling the aerosol chemistry. Highest concentrations of particulate K+, SO42-, NO3-, and NH4+ were observed at Hanoi in Vietnam. Correspondingly, highest AOD and AAOD were modeled at Bac Giang, also in Vietnam. The contribution of biomass burning to AOD was estimated to be over 56%, indicating the significant influence of biomass burning over this region. In Thailand, the magnitudes of major aerosol chemical components, AOD, and AAOD were much lower than in Vietnam. The contribution of biomass burning to AOD was about 18 - 50 %, indicating that Thailand was moderately impacted. In the downwind regions, the contribution of biomass burning to AOD at Hong Kong and Taiwan was significant within the range of 26% - 62%. The observed monthly mean SSA was around 0.90 during intense biomass burning periods, suggesting the great production of strongly absorbing substances (i.e, EC) due to biomass burning. Modeled concentrations of aerosol chemical components were biased low at most circumstances, and the modeled AOD values were biased low about a factor of 2, probably due to the underestimation of biomass burning emission.
Kan Huang
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Kirk Baker
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| 1:20 PM |
Robert Gilliam
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James Boylan
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| 1:40 PM |
Daniel Cohan
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Chris Emery
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| 2:00 PM |
Daiwen Kang
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Biswanath Chowdhury
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| 2:20 PM |
Tammy M. Thompson
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James Kelly
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| 2:40 PM |
Kazuyo Yamaji
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Application of the reactive plume model, SCICHEM-2012, to simulate near-source 1-hour NO2 concentrations Prakash Karamchandani, Ralph Morris, Greg Yarwood, Bart Brashers
ENVIRON International Corporation
Eladio Knipping
EPRI
Biswanath Chowdhury, Ian Sykes
Sage Management
SCICHEM is a state-of-the-science non-steady-state puff model with complete chemistry treatment, including gas-phase chemistry, aerosol chemistry, and cloud chemistry. It can be used for both local-scale and long-range transport applications. It accounts for the effects of building downwash on plume dispersion using the Plume Rise Model Enhancements (PRIME) algorithm. Several improvements have recently been made to SCICHEM, including enhancements to the dispersion component of the model, extensions to treat area sources and volume sources, an updated user-friendly interface (UFI) for setting up model applications, and updates to the chemistry modules. The model has also been adapted to read input files for AERMOD, the U.S. EPA regulatory model for short-range impacts. The new version of SCICHEM, referred to as SCICHEM-2012, will be available to the user community as a public domain model after it has been tested and evaluated. Here, we present the application of SCICHEM-2012 in a regulatory setting: the calculation of 1-hour NO2 concentrations to address the January 2010 short-term National Ambient Air Quality Standard (NAAQS) for NO2. We implemented gas-phase kinetic reactions for NO, NO2 and O3 in SCICHEM-2012 that are both scientifically rigorous, and suitable for such near-source, long-term applications. We use an AERMOD modeling database for a source that has difficulties demonstrating compliance with the 1-hour NO2 standard to conduct annual simulations with AERMOD and SCICHEM-2012. We compare the NO2/NOx ratios and maximum 1-hour NO2 concentrations predicted by the two models.
Prakash Karamchandani
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| 3:00 PM |
Break |
Break |
| 3:30 PM | Developer/User Meeting , moderated by Zac Adelman (UNC-Chapel Hill) Grumman Auditorium |
| 5:00 - 7:00 PM | Reception Atrium |
| October 17, 2012 |
| | Grumman Auditorium |
Dogwood Room |
| 7:30 AM | Registration and Continental Breakfast |
| 8:00 AM | A/V Upload for Oral Presenters | A/V Upload for Oral Presenters |
| |
Global/Regional Modeling Applications, chaired by Mike Moran (Environment Canada) and Rohit Mathur (US EPA) |
Source-Receptor Modeling and Analysis, chaired by Sergey Napelenok (US EPA) and Daniel Cohan (Rice University) |
| 8:30 AM |
Hyun Cheol Kim
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Carey Jang
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| 8:50 AM |
Mike Moran
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Kirk Baker
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| 9:10 AM |
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Wenxian Zhang
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| 9:30 AM |
Modeling Regional Ozone: A Comparison between a global and a regional model
Barron Henderson, Lin Zhang, Chris Emery and Joseph Pinto
Exposure to ozone is associated with a variety of health outcomes ranging from mild breathing discomfort to mortality. Ozone exposure fields are produced from precursors that can be broadly categorized as natural, intra-continental anthropogenic, and inter-continental anthropogenic. Understanding inter-continental contributions require global scale simulations. Understanding ozone exposure field features, however, requires finer spatial detail than can be supplied by most current global simulations. We compare the results from a nested version of the GEOS-Chem model (~ 50 km X 50 km resolution; Zhang et al. 2011) with that from CAMx (12 km X 12 km resolution; Emery et al. 2012) at CASTNET, AQS and NOAA monitoring sites for 2006. Both models are nested within a coarse resolution version of GEOS-Chem (~ 2° X 2.5°). Both models share similarities in simulated MDA8 O3. For example, both models indicate that intercontinental transport and stratospheric intrusions are the major sources of ozone in the intermountain West in spring; and in general when mean surface ozone is compared on a regional basis for averaging periods of a month or more, reasonable agreement is found between them and with measurements.
Most apparent differences between the models and with measurements occur at the ends of the concentration distribution (e.g., for 1st and 99th percentiles) on a day specific basis, e.g., both models show limited ability to capture the timing and strength of episodic sources such as stratospheric intrusions. They however, show better agreement with observations if the requirement of day specificity is removed, i.e., if episodic events are treated as stochastic. Even when day specificity is removed, differences between the simulations and between the simulations and observations persist. Some persistent differences are attributed to spatial resolution as expected. Others, however, can be attributed to the models representation of chemistry, their emissions from wildfires, and their production of NOx from lightning.
These results indicate that spatial resolution is not the only factor to be considered when attempting to simulate or attribute regional air quality. Rather, difference in models treatments of atmospheric chemistry and physics must be considered. These results are also in accord with earlier findings showing that agreement between models and measurements is improved as the averaging time of the simulation and measurements are increased. It is also apparent that in analyzing time series over long time periods (e.g., months), special care should be taken to examine temporal trends in bias as this will improve understanding of the processes in the model.
Emery, C.; Jung, J.; Downey, N.; Johnson, J.; Jimenez, M.; Yarwood, G.; Morris, R. Regional and global modeling estimates of policy relevant background ozone over the United States. Atmospheric Environment 2012, 47, 206217.
Zhang, L.; Jacob, D. J.; Downey, N. V.; Wood, D. A.; Blewitt, D.; Carouge, C. C.; van Donkelaar, A.; Jones, D. B. A.; Murray, L. T.; Wang, Y. Improved estimate of the policy-relevant background ozone in the United States using the GEOS-Chem global model with 1/2° × 2/3° horizontal resolution over North America. Atmospheric Environment 2011, 45, 67696776.
Barron Henderson
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Heather Simon
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| 9:50 AM |
Break |
Break |
| 10:20 AM |
Using Hemispheric-CMAQ to Provide Initial and Boundary Conditions for Regional Model Application
Joshua S. Fu1, Xinyi Dong1, Kan Huang1, Yang Gao1, and Carey Jang2
1Department of Civil and Environmental Engineering, The University of Tennessee, Knoxville, TN
2Office of Air Quality Planning and Standards, U.S. EPA, Research Triangle Park, NC
Initial and boundary condition (IC/BC) inputs for regional model are usually provided by global model through downscaling, for example, IC/BC derived from GEOS-Chem has been successfully employed in CMAQ applications for regional modeling (Lam and Fu, 2009). However, some limitations remain in the global model downscaling process, such as the stationary assumption within statistically downscaling limit the relationship between observation and models, and dynamic downscaling is usually computationally demanding and requires considerable implementation effort. In addition, the inconsistency between global and regional model in terms of both meteorology and chemical mechanisms may also introduce unrealistic chemical transports (Bullock et al., 2008; 2009). Therefore, it is necessary to extend the ability of regional model to conduct global scale of simulation and generate the nest-down IC/BC for regional applications. In this study, we are using CMAQ with polar stereographic projection for the whole North Hemisphere targeted to provide IC/BC for regional model application (HCMAQ).
The hemispheric modeling domain has horizontal resolution of 108km x 108km, and 34 vertical sigma-pressure coordinates with top height at 50 hPa. Meteorology filed is provided by WRF. Although emission inventories are available for regional application with CMAQ such as the National Emission Inventory (NEI) for US, the Intercontinental Chemical Transport Experiment-Phase B (INTEX-B) emission for China (Zhang et al., 2009), they are not directly used in this application because we want to examine the difference between HCMAQ and global model GEOS-Chem in terms of providing IC/BC, so emission dataset used in GEOS-Chem is extracted and re-projected for HCMAQ in order to keep the consistency between two different models. GEOS-Chem model simulation has been conducted for whole year 2008, and HCMAQ model simulation will be conducted for January and July 2008 for the first phase test run. Two sets of IC/BC will be derived for 36km US domain, one from GEOS-Chem results and the other from HCMAQ. These two sets will be compared to examine the difference caused by different chemical mechanisms, map projections, meteorological fields while generating IC/BC for regional application.
Reference:
Bullock, O.R., Jr., D. Atkinson, T. Braverman, K. Civerolo, A. Dastoor, D. Davignon, J-.Y. Ku, K. Lohman, T.C. Myers, R.J. Park, C. Seigneur, N.E. Selin, G. Sistla, K. Vijayaraghavan (2008), The North American Mercury Model Intercomparison Study (NAMMIS): Study description and model-to-model comparisons, J. of Geophys. Res., 113, D17310, doi:10.1029/2008JD009803
Bullock, O.R., Jr., D. Atkinson, T. Braverman, K. Civerolo, A. Dastoor, D. Davignon, J-.Y. Ku, K. Lohman, T.C. Myers, R.J. Park, C. Seigneur, N.E. Selin, G. Sistla, K. Vijayaraghavan (2009), An Analysis of Simulated Wet Deposition of Mercury from the North American Mercury Model Intercomparison Study (NAMMIS), J. of Geophys. Res., 114, D08301, doi:10.1029/2008JD011224
Lam Y.F. and J.S. Fu A novel downscaling technique for the linkage of global and regional air quality modeling, Atmos. Che. Phys., 9, 9169-9185, 2009
Zhang, Q., Streets, D. G., Carmichael, G. R., He, K. B., Huo, H., Kannari, A., Klimont, Z., Park, I. S., Reddy, S., Fu, J. S., Chen, D., Duan, L., Lei, Y., Wang, L. T., and Yao, Z. L.: Asian emissions in 2006 for the NASA INTEX-B mission, Atmos. Chem. Phys., 9, 5131-5153, 2009
Joshua Fu
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Farhan Akhtar
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| 10:40 AM |
Assessing the Impact of Changes in Climate and Emission on Global Air Quality
Timothy Glotfelty, Yang Zhang, and Shuai Zhu
Air Quality Forecasting Lab, North Carolina State University, Raleigh, NC
Prakash Karamchandani
ENVIRON International Corporation, Novato, CA
David G. Streets
Decision and Information Sciences Division, Argonne National Laboratory, Argonne, IL
The prospect of global climate change will have wide scale impacts in several areas, such as global/regional air/water quality, ecological stress, and human health. One aspect of concern is future changes in air quality that will result from changes in both meteorological forcing and air pollutant emissions. Two key air pollutants of interest include troposphereic ozone (O3) and atmospheric aerosols, due to their adverse effects on human health and feedbacks to the climate system. In this study the Global-through-Urban Weather Research and Forecasting Model with Chemistry (GU-WRF/Chem), is used to simulate current (2001 and 2010) and future (2020, 2030, 2040, and 2050) climate and emissions scenarios. The objectives of this study are to better understand the impact of future changes in meteorological forcing and emissions on global air quality and provide policy makers with scientific information for guidance in the creation of future air pollution and climate mitigation strategies. Projected anthropogenic emissions are based on the 3rd Assessment Report of the Intergovernmental Panel on Climate Change A1B Scenario, and biogenic emissions are calculated online using the Model of Emissions of Gases and Aerosols from Nature v. 2 (MEGAN2). Analysis of the simulation shows an increase in global 2-m temperature of 0.4-0.9 °C and global 2-m water vapor of 0.3 -0.4 g kg-1 between the current and future years. Seasonal average precipitation changes vary from near 0 mm day-1 in winter to increases of 0.03 mm day-1 in summer and autumn, with the largest differences associated with the shifts in tropical rain bands. The maximum 8-hr O3 level increases globally by 2-3 ppb as a result of increasing global temperatures and also increased emissions of nitrogen oxides and volatile organic compounds in India, eastern China, and Southeast Asia. The global fine particulate (PM2.5) level increases by 0.2-0.35 ¼g m-3 with differences being more regional in nature, which are associated with regional changes in the emissions of sulfur dioxide and primary particles. In response to increasing PM2.5 concentrations, cloud condensation nuclei will also increase over much of the globe with the exception of northern Eurasia and Central Africa in most seasons and at various super-saturations. There is a trend towards dimming at the earths surface as incoming solar radiation is reduced by 1.0-2.0 Wm-2; this results from a global
average increase in aerosol optical depth of 0.02-0.03 and cloud optical depth of 0.02-0.12 across the seasons. To conclude, under a future climate and emissions scenario, most of the world will experience deteriorating air quality from either increased 8-hr maximum O3, PM2.5, or both, with the largest increases of both pollutants in the India and Southeast Asia region. This underscores the need for synergetic efforts by policy makers at the international, national, and local levels to address the worldwide issues of climate mitigation and emissions control.
Timothy Glotfelty
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Shannon Capps
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| 11:00 AM |
Jared Bowden
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Amanda Pappin
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| 11:20 AM |
Russ Bullock
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Roger Kwok
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| 11:40 AM |
Improvement of extreme climate predictions from dynamical climate downscaling
Yang Gao1, Joshua S. Fu1, John B. Drake1, Yang Liu2, Jean-Francois Lamarque3, Kan Huang1, Xinyi Dong1 and David Wong4
1Department of Civil and Environmental Engineering, The University of Tennessee, Knoxville, TN
2Rollins School of Public Health, Emory University, Atlanta, Georgia
3Atmospheric Chemistry and Climate and Global Dynamics Divisions, National Center for Atmospheric Research, Boulder, CO
4Atmospheric Modeling and Analysis Division, NERL, USEPA, Research Triangle Park, NC
Due to the limitations of spatial resolution in global climate models, the mean climate studies are more preferable on a global scale. However, the extreme climate conditions play much more significant roles on human health. Thus, dynamical downscaling technique is used to link global and regional climate models. In this study, regional climate model Weather Research and Forecasting Model (WRF) was used to downscale three hourly global climate outputs from Community Earth System Model (CESM) version 1.0. The spatial resolution of CESM is 0.9 by 1.25 degree, while the resolutions of downscaled WRF domains are 36 km by 36 km and nested to 12 km and 4 km.
In this study, the present climate (2001-2004) and fossil fuel intensive scenario Coupled Model Intercomparison Project Phase 5 (CMIP 5) Representative Community Pathways (RCP) RCP 8.5 (2057-2059) was downscaled in order to determine future climate change. We first evaluated the predictions of extreme climate, including heat waves and flood between CESM and WRF. Compared with the observational data from National Climatic Data Center (NCDC), significant improvements in extreme events predictions were achieved after downscaling, and large bias was reduced in WRF in comparison to CESM. Compared to present climate, more intense heat waves and extreme rainfall will occur across the Eastern US.
Yang Gao
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Mike Barna
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| 12:00 PM |
Lunch, Trillium Room |
Lunch, Trillium Room |
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Global/Regional Modeling Applications, continued |
Air Quality Measurements and Observational Studies, chaired by Arastoo Pour Biazar (University of Alabama - Huntsville) |
| 1:00 PM |
Chris Nolte
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Airborne remote sensing of air quality over London and Western Europe: Validation and modelling of novel airborne FTIR-derived trace gas concentrations during the ClearFLo and MAMM campaigns.
Grant Allen, University of Manchester, UK
D. P. Moore, University of Leicester, UK
S. Newman, UK Met Office
A. Vance, UK Met Office
C. Percival, University of Manchester, UK
M. Gallagher, University of Manchester, UK
H. Coe, University of Manchester, UK
J. Lee, University of York, UK
J. McQuaid, University of Leeds, UK
Poor air quality in urban environments has been linked to premature death. Moreover, the ventilation of the urban boundary layer and impacts of advected urban pollution on the regional scale downwind may also contribute to adverse health effects in remote rural environments.
Airborne remote sensing of trace gases pertinent to air quality monitoring provide a measurement strategy that informs air quality models at both the urban and regional scales. In this study we present novel trace retrievals from an airborne FTIR - the Met Office Airborne Research Interferometer Evaluation System (ARIES). The new data provided by the ARIES instrument permits simultaneous nadir total column (and resolved profile) measurement of a wide range of trace gases (e.g. O3, CO2, H2O, N2O, CH4, HNO3) at ~1km spatial scale. Such data are well-suited to assimilation into air quality models and also serve as a useful validation of model output as well as facilitating inverse flux analyses.
Trace gas retrievals from ARIES will be presented in the context of simultaneous airborne and ground-based (in situ and remotely-sensed) data collected during the Clear Air For London (ClearFLo, July 2012) campaign and the Arctic Methane measurement and modelling (MAMM) campaign (July 2012). Both campaigns sample polluted airmasses in the urban environment and in the regional plume downwind, allowing excellent validation of the new retrieval strategy and a comprehensive dataset from which to conduct air quality modelling.
We will conclude by discussing planned applications of these measurements in flux determination and source-receptor analysis.
Grant Allen
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| 1:20 PM |
Development of a Regional-Scale Pollen Emission and Transport Modeling Framework for Investigating the Impact of Climate Change on Allergic Airway Disease
Rui Zhang1, Tiffany Duhl2, Muhammad T. Salam3, James M. House4, Richard C. Flagan4, Edward L. Avol3, Frank D. Gilliland3, Alex Guenther2, Serena H. Chung1, Brian K. Lamb1, and Timothy M. VanReken1
1Washington State University, Pullman, WA
2National Center for Atmospheric Research, Boulder, CO
3University of Southern California, Los Angeles, CA
4California Institute of Technology, Pasadena, CA
Exposure to bioaerosol allergens such as pollen can trigger allergic airway disease (AAD) for sensitive populations and thus can cause serious public health problems. Assessing these health impacts by linking the airborne pollen levels, concentrations of respirable allergenic material, and human allergenic response under current and future climate conditions is a key step toward developing effective preventive actions. To that end, a regional-scale pollen release and transport modeling framework has been developed that treats allergenic pollens as non-reactive tracers within the WRF/CMAQ air-quality modeling system. The pollen potential model, a module within the Model of Emissions of Gases and Aerosols from Nature (MEGAN), was developed to generate daily pool of pollen available for release. It is driven by species-specific meteorological threshold conditions (temperature and/or precipitation) and is flexible with respect to the representation of vegetation species and plant functional types. The hourly pollen emission flux was parameterized by considering available pollen grains, friction velocity and wind threshold values. The dry deposition velocity of each species of pollen was estimated based on pollen grain size and density.
An evaluation of this new pollen modeling framework was conducted over southern California for March to June 2010. This period coincided with observations by the University of Southern California's Children's Health Study (CHS), which included O3, PM2.5, and pollen count, as well as sensitization data at nine sites. Two nesting domains with horizontal resolution of 12 km and 4 km were constructed and six representative allergenic pollen genera were included: birch tree, walnut tree, mulberry tree, olive tree, oak tree, and brome grasses. Under the current parameterization scheme, the modeling framework tends to underestimate peaks in oak pollen concentration and overestimate grass pollen concentration, but it shows reasonable agreement with observed birch, olive, and mulberry tree pollen concentrations. Sensitivity studies suggested that the estimation of pollen available for release is a major source of uncertainty for simulated pollen concentrations. Achieving agreement between emission modeling and observed pattern of pollen releases is the key for successful pollen concentration simulations. The framework is being used to evaluate the impact of climate change on pollen release and concentration by comparing the simulation results with current decade (1995-2004) and future decade (2045-2054) WRF meteorological fields downscaled from the ECHAM5 global climate model results.
Rui Zhang
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Mohammed A Majeed
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| 1:40 PM |
Modeling Emission and Transport of Allergenic Tree Pollens under Climate Change
Yong Zhang1, Sastry Isukapalli1, Leonard Bielory2, Lai-yung Ruby Leung3, Panos G. Georgopoulos1
1 Environmental and Occupational Health Sciences Institute (EOHSI), A Joint Institute of UMDNJ-RW Johnson Medical School \& Rutgers University, 170 Frelinghuysen Road, Piscataway, NJ 08854, USA
2 Center for Environmental Prediction, Rutgers University, New Brunswick, NJ 08901, USA
3 Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA 99352, USA
Abstract: Climate change is expected to alter the emission and transport of allergenic pollens, and potentially increase occurrence of allergic airway disease (AAD). A modeling system is presented here for studying emission and transport of two representative allergenic tree pollens (birch and oak) under climatic change conditions. The emission module considers major physical processes such as direct emission and re-suspension of pollen particles, and accounts for meteorological parameters such as ground surface temperature, friction velocity, humidity, precipitation, etc. This module also incorporates statistical modeling based on historical data for estimating effects of climate change on annual flux and start date of pollen emissions. The transport of pollen was simulated via the combined application of the Weather Research and Forecasting (WRF) model, the Sparse Matrix Operator Kernel Emissions (SMOKE) model and an adapted version of Community Multiscale and Air Quality (CMAQ) model. Spatiotemporal profiles of pollen emissions and ambient airborne distributions in 2004, 2040 and 2050 were estimated through the combined application of (a) analysis results of historical data, (b) meteorological data from WRF under representative climate change scenarios, (c) land use and land cover data from Biogenic Emissions Land use Database, version 3 (BELD3). Simulation results of ambient distributions of pollen in 2004 were evaluated using observed pollen data from multiple pollen stations of the American Academy of Allergy, Asthma & Immunology (AAAAI). It is demonstrated that simulation results from the SMOKE-WRF-CMAQ modeling system could characterize reasonably well the spatiotemporal distribution of birch and oak pollen; and that the simulation estimates were comparable with those from observed climatologic means. It is also shown that responses of pollen timing and quantity to future climatic conditions will be different for different allergenic genus and different regions. Simulation results improve our understanding of climatic change effects on timing and quantity of emission and transport of allergenic pollens, and provide information useful in managing public health problems associated with expected increases in cases of AAD.
Keyword: Climate change, CMAQ, Pollen, Birch, Oak
Yong Zhang
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Michelle Snyder
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| 2:00 PM |
Tanya L. Otte
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Kenneth Pickering
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| 2:20 PM |
Break |
Break |
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Coupled Meteorology/Chemistry Models, chaired by Jon Pleim (US EPA) |
Air Quality Measurements and Observational Studies, continued |
| 2:50 PM |
Jonathan Pleim
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Tianfeng Chai
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| 3:10 PM |
Kiran Alapaty
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Pius Lee
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| 3:30 PM |
Shaocai Yu
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Annmarie Eldering
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| 3:50 PM |
Dr. P.A. Makar
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Arastoo Pour Biazar
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