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Recent Advances in Chemical Weather Forecasting in Support of Atmospheric Chemistry Field Experiments. Gregory R. Carmichael Department of Chemical & Biochemical Engineering Center for Global & Regional Environmental Research and the University of Iowa.
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Recent Advances in Chemical Weather Forecasting in Support of Atmospheric Chemistry Field Experiments Gregory R. Carmichael Department of Chemical & Biochemical Engineering Center for Global & Regional Environmental Research and the University of Iowa
Models are an Integral Part of Field Experiments • Flight planning • Provide 4-Dimensional context of the observations • Facilitate the integration of the different measurement platforms • Evaluate processes (e.g., role of biomass burning, heterogeneous chemistry….) • Evaluate emission estimates (bottom-up as well as top-down)
Satellite data in near-real time: MOPITT TOMS SEAWIFS AVHRR LIS TRACE-P EXECUTION Stratospheric intrusions FLIGHT PLANNING Long-range transport from Europe, N. America, Africa ASIAN OUTFLOW 3D chemical model forecasts: - ECHAM - GEOS-CHEM - Iowa/Kyushu - Meso-NH Boundary layer chemical/aerosol processing DC-8 P-3 PACIFIC • Emissions • Fossil fuel • Biomass burning • Biosphere, dust ASIA PACIFIC
ACE-Asia (NSF) & TRACE-P (NASA) Spring 2001 Experiments NASA/GTE DC-8
NASA GTE TRACE-P Mar’01-Apr’01 • Two aircrafts – DC8 and P3 • Chemical evolution during continental outflow, biomass burning, dust outbreaks, and urban plumes • 22 flights out of Hong Kong, Okinawa and Tokyo • O3, CO, SOx, NOx, HOx, RH and J • 100m to 12000m China
Model OverviewRegional Transport Model: STEM • Structure: Modular (on-line and off-line mode) • Meteorology: RAMS - MM5 - ECMWF - NCEP • Emissions: Anthropogenic, biogenic and natural • Chemical mechanism: SAPRC’99 (Carter,2000) • 93 Species, 225 reactions, explicit VOC treatment • Photolysis: NCAR-TUV 4.1 (30 reactions) • Resolution: Flexible 80km x 80km for regional and 16km x 16km for urban
Photochemistry: STEM-TUV Y. Tang (CGRER), 2002
Regional Emission Estimates:Anthropogenic Sources Industrial and Power Sector Coal, Fuel Oil, NG SO2, NOx, VOC, and Toxics Domestic Sector Coal, Biofuels, NG/LPG SO2, CO, and VOC Transportation Sector Gasoline, Diesel, CNG/LPG NOx, and VOC
Regional Emission Estimates:Natural Sources Biomass Burning In-field and Out-field combustion CO, NOx, VOC, and SPM Volcanoes SO2, and SPM Dust Outbreaks SPM
The Emissions Vary Greatly by Region – Reflecting Many Social/Economic Factors
The TRACE-P/Ace-Asia emission inventory shows the important sources of each type of air pollutant in Asia
For Southeast Asia and Indian Sub-Continent Original Fire Count(FC) data(AVHRR) 5-day Fire Count Moving Averaged Fire Count data (Level 2) “Fill-up” Zero Fire Counts using Moving Average(MA) Satellite Coverage Cloudiness Precipitation(NCEP) “Fill-up” Zero Fire Count using TOMS AI Mask Grid (Landcover) Mask Grid (Never Fire) “Extinguish” Fire Count using Mask Grids AI Adjusted Fire Count data (Level 3) Regress. Coeff.(AI/FC) Regional Emission Estimates:Biomass Burning Emissions
Open Burning Emissions of CO – Based on AVHRR Fire-count Data
Comparison of country surveys with various AVHRR fire-count adjustments reveals problem areas for further investigation Xinjiang Mongolia fire count > country surveys India fire count < country surveys Vietnam Indonesia It remains difficult to make the link between satellite observations of fire and atmospheric emissions
The Importance of Fossil, Biofuels and Open Burning Varies by Region
Uncertainty analysis has revealed wide differencesin our knowledge of the emissions of particularspecies in particular parts of Asia …
March 9 --forecast 3/9 Example of Forecast Used in Flight Planning
Frontal outflow of biomass burning plumes E of Hong Kong Biomass burning CO forecast (G.R. Carmichael, U. Iowa) Observed CO (G.W. Sachse, NASA/LaRC) Observed aerosol potassium (R. Weber, Georgia Tech)
Using Measurements and Model – We Estimate Contributions of Fossil, Biofuel and Open Burning Sources
Testing Model:CO under-prediction under 1000m for TRACE-P ---WHY? What doe this tell us ? CO data from Sacshe
Back Trajectories from High CO point. --- CO > 700 --- CO > 600 --- CO > 500 --- CO > 450 --- CO > 400
Back Trajectories from High CO point(Zoom & CO > 500 ppbv) --- CO > 700 --- CO > 600 --- CO > 500
Urban PhotochemistryOH Radical Cycle VOC + OH ---> Orgainic PM PM2.5 SOx [or NOx] + NH3 + OH ---> (NH4)2SO4 [or NH4NO3] Ozone Visibility Fine PM (Nitrate, Sulfate, Organic PM) .OH NOx + VOC + OH + hv ---> O3 Acid Rain Water Quality SO2 + OH ---> H2SO4 NOx + SOx + OH (Lake Acidification, Eutrophication) NO2 + OH ---> HNO3 Air Toxics OH <---> Air Toxics (POPs, Hg(II), etc.)
Urban/Regional Photochemistry • Tropospheric chemistry is characterized by reaction cycles • OH plays a key role in tropospheric chemistry • Reactions lead to removal as well as generation of pollutants • NOx to VOC ratio governs Ozone production
Urban/Regional PhotochemistryNOx-VOC-Ozone Cycle • Organic radical production and photolysis of NO2 • VOC’s and N-species compete for OH radical
Urban/Regional PhotochemistryNOx-VOC-Ozone Cycle • In polluted environment, CO contributes to O3 production
Urban/Regional PhotochemistryNOx-VOC-Ozone Cycle • HCHO – primary intermediate in VOC-HOx chemistry • Short lived and indicator of primary VOC emissions
Comparison of Observed and Modeled OH Provides a Direct Check on Models
Characterization of Urban PollutionFlight DC8-13 : 03/21/2001 Flight Path Back Traj. % Urban HCHO • 1000 ppbv of CO, 10 ppbv of HCHO, 100 ppbv of O3 • Fresh plumes out of Shanghai, < 0.5 day in age
We run back-trajectories from each 5 minute leg of merge data set. Keep track of each time a trajectory passes in the grid cell of the city and below 2 km. Classification of trajectory by the Source of Megacity. Age as determined by trajectory is also shown Before Big difference !!! We catch more number of fresh airmass from Shanghai and Seoul.
Comparing Modeled and Measured Ratios We extract all points associated with a specified city and plot measured ratios and plot modeled ratios.
Comparison of Modeled and Observed Results from China’s Mega Cities
Urban Photochemistry HCHO to CO Ratios Age in days calculated from back trajectories along the flight path Units: ppbv-HCHO/ ppbv-CO
Ratio Analysis by Back trajectory region category. (1) Only from 01-05GMT Japan Central China (Shanghai etc) ΔO3/ΔNOz
Urban Photochemistry NOx-VOC Sensitivity to O3 Production Less than 2 day old plumes VOC sensitive Model results along the flight path Megacity points from back trajectories Loss(N)/(Loss(N)+Loss(R)) NOx sensitive Model NOx (ppbv) Klienman et al., 2000
Rishiri DUST[μg/m3] Lev =10,30,60,90,120,150,180,210 10 227 8 8 8 6 6 6 Height[km] Height[km] Height[km] 4 4 4 2 2 2 E90 E120 E150 SO4 [μg/m3] Lev =1,3,6,9,12,15,18,21 1 21.2 0 0 0 Rishiri Tarukawa Sado Harbin Beijing Tsukuba BC[μg/m3] Lev =0.1,0.24,0.36,0.48,0.6,0.72,0.84,0.96,1.08 0.1 1.15 Hachijo N30 Qingdao :BC+OC :DUST OC[μg/m3] 0.1 3.48 Lev =0.1,0.4,0.8,1.2,1.6,2.0,2.4,2.8,3.2 Shanghai :Sea salt 8 Ogasawara 6 Height[km] Nagasaki & Fukue 4 2 :Sulfate 0 Okinawa Fukuoka Amami AOD E.Q. APRIL
Analysis Framework Climate : Air Quality