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Envair DRI Alpine Geophysics

Understanding Relationships Between Changes in Ambient Ozone and Precursor Concentrations and Changes in VOC and NOx Emissions from 1990 to 2004 in Central California. Envair DRI Alpine Geophysics. May 25, 2006. Today’s Meeting – Progress Report. Data acquisition and evaluation

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Envair DRI Alpine Geophysics

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  1. Understanding Relationships Between Changes in Ambient Ozone and Precursor Concentrations and Changes in VOC and NOx Emissions from 1990 to 2004 in Central California Envair DRI Alpine Geophysics May 25, 2006

  2. Today’s Meeting – Progress Report • Data acquisition and evaluation • Met classification results (version 2) • Ambient AQ trends • Next steps • Feedback?

  3. Data Acquisition and Evaluation

  4. Emissions Inventories • Obtained ARB monthly historical emissions • Have checked completeness & readability • Status: ready for re-aggregation into county or greater total VOC, NOx, CO

  5. Ambient AQ Data • Hourly gas-phase (O3, NO, NOx, CO, HC) • Completeness • Rounding conventions • VOC: PAMS, ARB, SJVAQS (1990) • No combination of previous VOC validation provides complete spatial & temporal coverage • Start with EPA archives and validate data

  6. Meteorological Data • Upper air: Oakland soundings 4 am & 4 pm • Pressure gradients: San Francisco to Medford, Reno, and Fresno • Surface wind speed and direction (applied QA steps recommended by BAAQMD)

  7. Surface Met Data QA Issues Identified by BAAQMD • Site locations • Time zone • Zero values vs. missing data • Sudden increases or decreases in WS, T • Long periods of constant WS, WD, or T • Incorrect flag values • Redundant data

  8. Surface Meteorological Stations

  9. Met Classification Methods

  10. Met Classification Approach • Goal is to stratify days, not to adjust ozone • Stratifications related to transport directions • Primary clustering method is based on met variables related to transport • Secondary method is spatial correlation of peak ozone (e.g., DRI CCOS clustering algorithm, BAAQMD analysis)

  11. Met Classification Details • K-means clustering • Use all days May through October each year • Standardized variables • 850 mb T, height, u and v wind vector components • Pressure gradients SFO to Medford, Reno, Fresno • Surface u and v wind vector components, 53 stations • Limited to 12 cluster types

  12. Classification Results

  13. Summary of Findings • Met classifications yield clusters having differences in transport direction or distance • Different clusters exhibit different mean concentrations of air pollutants • Pollutant trends at a site may but do not always differ among clusters • Clusters account for about 30 – 40% of ozone variance

  14. Four Met Types Dominate Jul - Oct

  15. Which Clusters Have Highest Ozone? • Clusters 1, 3, 5, 6 (summer and fall) • Sometimes cluster 9 (Sep and Oct) • In southern SJV, also clusters 2, 7, 8, 11 (occur most frequently May and June)

  16. Daily 8-Hour Peak Ozone, 1990-2004Livermore Meteorological Type (cluster number)

  17. Daily 8-Hour Peak Ozone, 1990-2004Folsom Meteorological Type (cluster number)

  18. Daily 8-Hour Peak Ozone, 1990-2004Parlier Meteorological Type (cluster number)

  19. Daily 8-Hour Peak Ozone, 1990-2004Arvin Meteorological Type (cluster number)

  20. Do clusters exhibit differences in transport direction and distance? … most easily seen using plots of U and V wind vector components (these show direction of origin)

  21. Directional Differences

  22. Directional Differences

  23. Directional Differences

  24. Directional Differences

  25. Mean Directional Differences

  26. 850 mb Directional Differences

  27. Directional Differences

  28. Main Finding of Cluster Analysis Clusters exhibit differences in transport directions or distances. The differences are more pronounced at some sites than others.

  29. Can Clusters Be Improved? Maybe - Direct comparisons of met types (clusters) to groupings determined from wind speed and direction at each site suggest room for improvement.

  30. Chabot 12 1 4 2 8 11 1 4 2 10 11 1 4 10 1 42 10 9 36 24 20 1 3 5 8 1 2 21 4 62 5 Cluster 7 1 100 5 6 16 5 166 23 5 1 3 31 126 4 4 7 4 16 2 3 12 64 109 44 55 2 6 2 41 12 1 83 8 1 12 34 3 2 5 Calm <1m/s NE 1-2m/s SE 1-2m/s SW 1-2m/s NW 1-2m/s NE >2m/s SE >2m/s SW >2m/s NW >2m/s Direction/Windspeed

  31. Sacramento 12 2 1 38 11 1 62 10 7 4 9 1 5 69 2 9 24 9 55 1 99 8 20 5 85 23 7 82 12 Cluster 7 1 3 18 233 6 6 5 59 30 319 5 22 16 286 4 16 1 10 7 25 21 3 148 26 207 19 14 131 2 3 5 5 157 1 212 1 13 27 41 6 12 1 Calm <1m/s NE 1-2m/s SE 1-2m/s SW 1-2m/s NW 1-2m/s NE >2m/s SE >2m/s SW >2m/s NW >2m/s Direction/Windspeed

  32. Fresno 12 1 40 11 39 1 13 6 10 3 1 12 79 9 77 1 1 90 15 8 2 30 198 Cluster 7 3 18 2 231 6 25 1 1 226 1 159 5 79 2 7 196 50 4 38 1 15 5 3 13 3 3 346 1 2 2 186 5 2 30 1 2 4 71 59 1 290 3 1 6 Calm <1m/s NE 1-2m/s SE 1-2m/s SW 1-2m/s NW 1-2m/s NE >2m/s SE >2m/s SW >2m/s NW >2m/s Direction/Windspeed

  33. Preliminary Trends Assessment

  34. Trends Methods • Split subregional top 60 days by cluster • For each site and each cluster, compute linear regression of AQ metric against day • Determine regression slope and SE

  35. Do trends differ among clusters?

  36. CO Trends

  37. Daily Morning CO – All Sites

  38. Error bars = 2 SE of slope

  39. Error bars = 2 SE of slope

  40. Error bars = 2 SE of slope

  41. Error bars = 2 SE of slope

  42. Error bars = 2 SE of slope

  43. Error bars = 2 SE of slope

  44. Error bars = 2 SE of slope

  45. Error bars = 2 SE of slope

  46. Error bars = 2 SE of slope

  47. NOx Trends

  48. Daily Morning NOx – All Sites

  49. Error bars = 2 SE of slope

  50. Error bars = 2 SE of slope

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