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Premium member Presentation Transcript Slide1: CCOS 2000 Model Intercomparison: Diagnostic Analyses January 27 2002, Progress Report to CARB Gail Tonnesen, Zion Wang, Mohammad Omary, Bo Wang University of California, Riverside Bourns College of Engineering Center for Environmental Research and TechnologyProcess Analysis Outputs for CAMx: Process Analysis Outputs for CAMx Integrated reaction rates (IRR) show chemical production and loss in the grid cell where the species reacted. Results shown here as total ppb/day Integrated Process Rates (IPR) show transport, dispersion, emissions, deposition. Have not looked at these terms yet.Chemical Process Analysis for CAMx: Chemical Process Analysis for CAMx IRR outputs stored in CAMx CPA file: Total reactivity P(Ox) = P(O3) and oxidation of NO. Radical budget controls P(O3) and sensitivity in urban areas: Radical initiation Radical propagation and termination NOy budget controls P(O3) and O3 sensitivity in rural areas: Conversion of NOx to Inert HNO3, RNO3, PAN. CAMx CB4 vs SAPRC99 reactivity: CAMx CB4 vs SAPRC99 reactivity As expected SAPRC99 is “hotter”than CB4: SAPRC99 has greater organic radical production and lower OH+NO2 radical termination. SAPRC99 produces more O3 in urban areas and less in rural areas. Consistent with box model comparisons. Next several plots compare P(Ox) reactivity in CAMx CB4 and SAPRC99 and also show day to day variability in reactivity.CAMx P(Ox) on July 30: CAMx P(Ox) on July 30CAMx P(Ox) on July 30: CAMx P(Ox) on July 30CAMx P(Ox) on July 31: CAMx P(Ox) on July 31CAMx P(Ox) on August 1: CAMx P(Ox) on August 1CAMx P(Ox) on August 2: CAMx P(Ox) on August 2Production of HNO3 by OH+NO2 on July 30: Production of HNO3 by OH+NO2 on July 30Production of HNO3 by N2O5 on July 30: Production of HNO3 by N2O5 on July 30Production of RNO3 on July 30: Production of RNO3 on July 30Net Production of PANs on July 30: Net Production of PANs on July 30Production efficiency P(Ox)/P(NOz): Production efficiency P(Ox)/P(NOz)Slide15: O3 VOC-NOx Sensitivity Use observation based methods to estimate peak O3 sensitivity to VOC and NOx Compare grid model with constrained steady state model results. Use process analysis to estimate P(Ox) sensitivity to VOC and NOx.H2O2/HNO3 for CB4 July 30: H2O2/HNO3 for CB4 July 30H2O2/HNO3 for SAPRC99 July 30: H2O2/HNO3 for SAPRC99 July 30H2O2/HNO3 for CB4 July 31: H2O2/HNO3 for CB4 July 31H2O2/HNO3 for SAPRC99 July 31: H2O2/HNO3 for SAPRC99 July 31H2O2/HNO3 for CB4 August 1: H2O2/HNO3 for CB4 August 1H2O2/HNO3 for SAPRC99 August 1: H2O2/HNO3 for SAPRC99 August 1H2O2/HNO3 for CB4 August 2: H2O2/HNO3 for CB4 August 2O3 Sensitivity versus P(O3) Sensitivity: O3 Sensitivity versus P(O3) SensitivityExtent Parameter: Extent Parameter Calculated extent using ambient data as average of measured NOx = NO+NO2 and measured NOx = NOy. Calculated model extent as NOx=NO+NO2. Poor agreement between models and data. Need to further evaluate this. Extent from Ambient O3-NOx data: Extent from Ambient O3-NOx dataExtent from Ambient O3-NOx data: Extent from Ambient O3-NOx dataExtent at Parlier Site July 30(NO2 from TDL): Extent at Parlier Site July 30 (NO2 from TDL)Extent at Parlier Site July 31(NO2 from TDL): Extent at Parlier Site July 31 (NO2 from TDL)Extent at Parlier Site August 1(NO2 from TDL): Extent at Parlier Site August 1 (NO2 from TDL)Extent at Parlier Site August 2(NO2 from TDL): Extent at Parlier Site August 2 (NO2 from TDL)Evaluate Vertical Mixing: Evaluate Vertical Mixing Comparsions of CO as a relatively inert tracer Sensitivity run with met pass through for CMAQModel CO Conc Differences: Model CO Conc Differences CMAQ has lower conc early morning and higher conc later in the day. Hypothesis: Difference in vertical dispersion CO Conc plots do not appear to support this. Need to further investigate.Model CO at 5:00 PDT: Model CO at 5:00 PDTModel CO at 6:00 PDT: Model CO at 6:00 PDTSlide35: Model CO at 8:00 PDTModel CO at 10:00 PDT: Model CO at 10:00 PDTSlide37: Model CO N-S Slice at 8:00 PDTCMAQ MCIP2 Sensitivity: CMAQ MCIP2 Sensitivity Pass through of MM5 MRF Met dataRecommendations: Recommendations Focus primarily on CAMx with SAPRC99 for the next phase of modeling. Continue to investigate CMAQ Meteorology and vertical mixing, h-diffusion Updated N2O5 HNO3 with aerosols Additional CMAQ runs well be useful for corrobatory analysis. Run both models again if there are substantial changes in emissions.Slide40: Next Steps Update emissions inventories Updated Mobile inventory Corrections to point sources Resolve discrepancy in emissions processing CAMx sensitivity runs with lower model top, approx 4 km to reduce number of vertical layers. CMAQ Need aerosol chemistry to use updated N2O5 kinetics Investigate vertical mixing and horizontal diffusion You do not have the permission to view this presentation. In order to view it, please contact the author of the presentation.
ccos diagnostic Teobaldo Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 92 Category: Education License: All Rights Reserved Like it (0) Dislike it (0) Added: February 29, 2008 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Slide1: CCOS 2000 Model Intercomparison: Diagnostic Analyses January 27 2002, Progress Report to CARB Gail Tonnesen, Zion Wang, Mohammad Omary, Bo Wang University of California, Riverside Bourns College of Engineering Center for Environmental Research and TechnologyProcess Analysis Outputs for CAMx: Process Analysis Outputs for CAMx Integrated reaction rates (IRR) show chemical production and loss in the grid cell where the species reacted. Results shown here as total ppb/day Integrated Process Rates (IPR) show transport, dispersion, emissions, deposition. Have not looked at these terms yet.Chemical Process Analysis for CAMx: Chemical Process Analysis for CAMx IRR outputs stored in CAMx CPA file: Total reactivity P(Ox) = P(O3) and oxidation of NO. Radical budget controls P(O3) and sensitivity in urban areas: Radical initiation Radical propagation and termination NOy budget controls P(O3) and O3 sensitivity in rural areas: Conversion of NOx to Inert HNO3, RNO3, PAN. CAMx CB4 vs SAPRC99 reactivity: CAMx CB4 vs SAPRC99 reactivity As expected SAPRC99 is “hotter”than CB4: SAPRC99 has greater organic radical production and lower OH+NO2 radical termination. SAPRC99 produces more O3 in urban areas and less in rural areas. Consistent with box model comparisons. Next several plots compare P(Ox) reactivity in CAMx CB4 and SAPRC99 and also show day to day variability in reactivity.CAMx P(Ox) on July 30: CAMx P(Ox) on July 30CAMx P(Ox) on July 30: CAMx P(Ox) on July 30CAMx P(Ox) on July 31: CAMx P(Ox) on July 31CAMx P(Ox) on August 1: CAMx P(Ox) on August 1CAMx P(Ox) on August 2: CAMx P(Ox) on August 2Production of HNO3 by OH+NO2 on July 30: Production of HNO3 by OH+NO2 on July 30Production of HNO3 by N2O5 on July 30: Production of HNO3 by N2O5 on July 30Production of RNO3 on July 30: Production of RNO3 on July 30Net Production of PANs on July 30: Net Production of PANs on July 30Production efficiency P(Ox)/P(NOz): Production efficiency P(Ox)/P(NOz)Slide15: O3 VOC-NOx Sensitivity Use observation based methods to estimate peak O3 sensitivity to VOC and NOx Compare grid model with constrained steady state model results. Use process analysis to estimate P(Ox) sensitivity to VOC and NOx.H2O2/HNO3 for CB4 July 30: H2O2/HNO3 for CB4 July 30H2O2/HNO3 for SAPRC99 July 30: H2O2/HNO3 for SAPRC99 July 30H2O2/HNO3 for CB4 July 31: H2O2/HNO3 for CB4 July 31H2O2/HNO3 for SAPRC99 July 31: H2O2/HNO3 for SAPRC99 July 31H2O2/HNO3 for CB4 August 1: H2O2/HNO3 for CB4 August 1H2O2/HNO3 for SAPRC99 August 1: H2O2/HNO3 for SAPRC99 August 1H2O2/HNO3 for CB4 August 2: H2O2/HNO3 for CB4 August 2O3 Sensitivity versus P(O3) Sensitivity: O3 Sensitivity versus P(O3) SensitivityExtent Parameter: Extent Parameter Calculated extent using ambient data as average of measured NOx = NO+NO2 and measured NOx = NOy. Calculated model extent as NOx=NO+NO2. Poor agreement between models and data. Need to further evaluate this. Extent from Ambient O3-NOx data: Extent from Ambient O3-NOx dataExtent from Ambient O3-NOx data: Extent from Ambient O3-NOx dataExtent at Parlier Site July 30(NO2 from TDL): Extent at Parlier Site July 30 (NO2 from TDL)Extent at Parlier Site July 31(NO2 from TDL): Extent at Parlier Site July 31 (NO2 from TDL)Extent at Parlier Site August 1(NO2 from TDL): Extent at Parlier Site August 1 (NO2 from TDL)Extent at Parlier Site August 2(NO2 from TDL): Extent at Parlier Site August 2 (NO2 from TDL)Evaluate Vertical Mixing: Evaluate Vertical Mixing Comparsions of CO as a relatively inert tracer Sensitivity run with met pass through for CMAQModel CO Conc Differences: Model CO Conc Differences CMAQ has lower conc early morning and higher conc later in the day. Hypothesis: Difference in vertical dispersion CO Conc plots do not appear to support this. Need to further investigate.Model CO at 5:00 PDT: Model CO at 5:00 PDTModel CO at 6:00 PDT: Model CO at 6:00 PDTSlide35: Model CO at 8:00 PDTModel CO at 10:00 PDT: Model CO at 10:00 PDTSlide37: Model CO N-S Slice at 8:00 PDTCMAQ MCIP2 Sensitivity: CMAQ MCIP2 Sensitivity Pass through of MM5 MRF Met dataRecommendations: Recommendations Focus primarily on CAMx with SAPRC99 for the next phase of modeling. Continue to investigate CMAQ Meteorology and vertical mixing, h-diffusion Updated N2O5 HNO3 with aerosols Additional CMAQ runs well be useful for corrobatory analysis. Run both models again if there are substantial changes in emissions.Slide40: Next Steps Update emissions inventories Updated Mobile inventory Corrections to point sources Resolve discrepancy in emissions processing CAMx sensitivity runs with lower model top, approx 4 km to reduce number of vertical layers. CMAQ Need aerosol chemistry to use updated N2O5 kinetics Investigate vertical mixing and horizontal diffusion