1 Air Quality Reanalysis (Configuration for 2010 HTAP production) AQAST-9 June 2-4, 2015, St Louis, MO Greg Carmichael 1, Pius Lee 2, Brad Pierce 3, Dick.

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Presentation transcript:

1 Air Quality Reanalysis (Configuration for 2010 HTAP production) AQAST-9 June 2-4, 2015, St Louis, MO Greg Carmichael 1, Pius Lee 2, Brad Pierce 3, Dick McNider 4, Ted Russell 5, Edward Hyer 6, Yang Liu 7, Arastoo Pour Biazar 4, Yongtao Hu 5, Talat Odman 5, Scott Spak 1, David Edwards 8, Ken Pickering 9, Youhua Tang 2, Li Pan 2, Hyuncheol Kim 2, Daniel Tong 2 1 College of Engineering, University of Iowa, Iowa City, IA 2 Air Resources Lab., NOAA Center for Weather and Climate Prediction, College Park, MD 3 National Environmental Satellite and Information Service (NESDIS), Madison, WI 4 Department of Atmospheric Science, University Alabama, Huntsville AL 5 School of Civil and Environmental Engr., Georgia Institute of Technology, Atlanta, GA 6 Naval Research Laboratory, Monterey, CA 7 Department of Environmental Health, Emory University, Atlanta, GA 8 Corporation for Atmospheric Research, Boulder, CO 9 Atmospheric Chemistry and Dynamics Lab., NASA, Greenbelt MD

Courtesy: Dan Costa “New Directions in Air Quality Research at the US EPA” 2 AQAST-9 June 2-4, 2015, St Louis, MO

33 Outline on progress  The Regional Chemical Analysis TT started in 2013:  Deliverable in 2014: Analysis fields for July 2011 provided for GaTech and UMD for SIP modeling o Assimilated exo-domain wild fire, O 3 using RAQM o Upgrade emission based on NEI2011 o Assimilated wild-fire using NESDIS obs, PM 2.5 constraints using MODIS AOD & AQS PM 2.5 o Assimilated cloud attenuated photolytic rate o Mimicked SIP reduced RMSE by 400% for PM 2.5  Deliverable in 2015: Analysis fields for 2010, support HTAP o Assimilate lightning NOx, PAR, DYNAMO Isoprene  User friendly portal and archive for chemical analysis fields over Continental U.S. AQAST-9 June 2-4, 2015, St Louis, MO

4 Constrained Satellite Products Global Assimilation + AQ Assessments + State Implementation Plan Modeling + Rapid deployment of on- demand rapid- response forecasting; e.g., new fuel type,…, etc. + Health Impacts assessments + Demonstration of the impact of observations on AQ distributions + Ingestion of new AQAST products into operations AQAST Project: Air Quality Reanalysis ( Translating Research to Services ) 3:30-5:00 Session Yang Liu: MODIS C6 Alvarado & Hegarty: NH 3 Huang, McNide, Lee : T Skin AQAST-9 June 2-4, 2015, St Louis, MO

5 Applications of Reanalysis Reanalysis would be able to provide PM2.5 speciation data with national coverage at county level AQAST-9 June 2-4, 2015, St Louis, MO

 NOMADS  RSIG. NOAA Service: A user friendly downloadable archive 6 analysis New AQAST-9 June 2-4, 2015, St Louis, MO

7 Comparison of Wind along flight track of P3B on July Spirals over Wilmington and Edgewood Model under-predicted wind shear Lee & Liu, 2014 Int.J.Environ. Res. Public H. Time labels in transact Pickering and Lee, 2014 Environ. Manager AQAST-9 June 2-4, 2015, St Louis, MO

8 Lightning NOx AIRNow Cloud-obs Photolysis rates Isoprene & PAR done Yet to do New AQAST-9 June 2-4, 2015, St Louis, MO

Lightning Process currently used in CMAQ 5.0* *CMAQ Version 5.0 and higher contains a scheme based on Allen et al. (2012, ACP) that was funded under NASA Applied Sciences Air Quality Program project (Ken Pickering, PI):  Method for estimating lightning flash rates  LNO x production per flash  Method of allocating LNO x production in the vertical NLDN (National Lightning Detection Network) data Map to CMAQ grid Calculate Total monthly Lightning flash Count over each grid Model’s convective Precipitation rate Model’s strike count (monthly total) Mean LTratio used in CMAQ NLDN/Model AQAST-9 June 2-4, 2015, St Louis, MO 9

July 1-10, 2011 NO 2 (Left) Base (Right) with LNOx, (Bottom) Difference Midwest convections. GOES13 AQAST-9 June 2-4, 2015, St Louis, MO 10

July 1-10, 2011 O 3 (Left) Base (Right) with LNOx, (Bottom) Verification AQAST-9 June 2-4, 2015, St Louis, MO O 3 10 days avgStationsObs meanMean biasRMSECorr. Coef. Base O 3 10 days avg (RM)StationsObs meanMean biasRMSECorr. Coef. Base Include LNOx

AQAST-9 June 2-4, 2015, St Louis, MO July 1-10, 2011 PM 2.5 (Left) Base (Right) with LNOx, (Bottom) Verification PM days avgStationsObs meanMean biasRMSECorr. Coef. Base PM days avg (UM)StationsObs meanMean biasRMSECorr. Coef. Base Include LNOx

13  The analysis forward model is tested and used to generate July 2011 analysis fields.  July 2011 analysis fields was used by Georgia Tech for a 14-day SIP simulation and showed significant improvement in RMSE  Data Set assimilated: RAQMS (MLS, OMI O 3, MODIS AOD); HMS Fire; GOES cloud fraction for photolytic rate correction; MODIS AOD; AQS O 3, PM 2.5  Assimilate lightning NOx: Use NOAA hourly reporting of the National Lightning Detection Network to derive and distribute LNOx  Preliminary surface NOx and O 3 verification showed over-estimation  Further improvement of LNOx assimilation algorithm is being test  Analysis configuration also includes observation set on biogenic emission from the DYNAMO team  Production FY2010 in conjunction with HTAP support  Portal via RSIG is being tested Summary AQAST-9 June 2-4, 2015, St Louis, MO Tong and Lee et al. 2015: “NO x trends over large cities”, Atmos. Environ Pan and Lee et al. 2014: “Forecasting performance of NAQFC”, Atmos. Environ

7 th International Workshop on Air Quality Forecasting Research September NOAA NCWCP, College Park, MD

Deep Convective Clouds and Chemistry (DC3) Case Study – May 29-30, 2012 Multicell storm in NW Oklahoma in early evening of May 29 sampled by NASA DC-8 and NCAR G-V; storm simulated using WRF-Chem at 1-km resolution Model-calculated reflectivity and aircraft tracks Trajectories show transport of storm outflow to Southern Appalachians by early afternoon May 30, where NO 2 peak was detected by OMI and DC3 research aircraft Courtesy: Pickering, Cummings, Allen WRF-Chem -- Vertical Cross Section for NO x WRF-Chem (cloud-resolved) 0100 UTC AQAST-9 June 2-4, 2015, St Louis, MO 15

LNO x Production Per Flash: 500 moles NO x per flash assumed for continental US based on INTEX-A GEOS-Chem results (e.g., Hudman et al., 2007, JGR) and cloud-resolved model simulations for individual storms constrained by anvil aircraft observations from several field programs (Ott et al., 2010, JGR) However, estimates of LNO x production from OMI observations over the Gulf of Mexico and surrounding coastal regions are ~190 to 250 moles per flash (Pickering et al., 2015, JGR, to be submitted) User can modify moles per flash for IC and CG flashes Vertical Distribution of LNO x Production: Based on Koshak et al. (2014, Atmos. Res.) vertical distributions of lightning channel lengths from Northern Alabama Lightning Mapping Array -- work sponsored by NASA Applied Science Air Quality Program AQAST-9 June 2-4, 2015, St Louis, MO 16

MODIS (Moderate Resolution Imaging Spectroradiometer) AOD Orbit:705 km, 10:30 a.m. descending node (Terra) or 1:30 p.m. ascending node (Aqua) Swath Dimensions: 2330 km (cross track) by 10 km (along track at nadir) Spatial Resolution: 250 m (bands 1-2) 500 m (bands 3-7) 1000 m (bands 8-36) Courtesy :NESDIS 17 National correlation map between AIRNow measurement and MODIS AOD Typically good correlation between surface PM 2.5 and AOD retrieved by MODIS Typically good correlation between surface PM 2.5 and AOD retrieved by MODIS AQAST-9 June 2-4, 2015, St Louis, MO

Optimal Interpolation (OI) OI simplifies the extended Kalman filter formulation (Dee et al. Q. J. R. Meteor. Soc. 1998) by limiting the analysis problem to a subset of obs. Obs far away (beyond background error correlation length scale) have no effect in the analysis. Injection of Obs through OI takes place at 1800 UTC daily. 18 AQAST-9 June 2-4, 2015, St Louis, MO