envair dri alpine geophysics

133
Copyright © 2009 – The McGraw-Hill Companies srl Capitolo 8 Massimizzazione dei profitti

Upload: faxon

Post on 14-Jan-2016

32 views

Category:

Documents


0 download

DESCRIPTION

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 - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: 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

Page 2: Envair DRI Alpine Geophysics

2

Today’s Meeting – Progress Report

Data acquisition and evaluation Met classification results (version 2) Ambient AQ trends Next steps Feedback?

Page 3: Envair DRI Alpine Geophysics

3

Data Acquisition and Evaluation

Page 4: Envair DRI Alpine Geophysics

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

Page 5: Envair DRI Alpine Geophysics

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

Page 6: Envair DRI Alpine Geophysics

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)

Page 7: Envair DRI Alpine Geophysics

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

Page 8: Envair DRI Alpine Geophysics

8

Network

N CD C

C IM IS

BAAQ M D

Sites w ith 10 + years of M eteorological Data (daily w indspeed and w ind direction)

Surface MeteorologicalStations

Page 9: Envair DRI Alpine Geophysics

9

Met Classification Methods

Page 10: Envair DRI Alpine Geophysics

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)

Page 11: Envair DRI Alpine Geophysics

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

Page 12: Envair DRI Alpine Geophysics

12

Classification Results

Page 13: Envair DRI Alpine Geophysics

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

Page 14: Envair DRI Alpine Geophysics

14

Four Met Types Dominate Jul - Oct

Page 15: Envair DRI Alpine Geophysics

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)

Page 16: Envair DRI Alpine Geophysics

16

Daily 8-Hour Peak Ozone, 1990-2004Livermore

Meteorological Type (cluster number)

Page 17: Envair DRI Alpine Geophysics

17

Daily 8-Hour Peak Ozone, 1990-2004Folsom

Meteorological Type (cluster number)

Page 18: Envair DRI Alpine Geophysics

18

Daily 8-Hour Peak Ozone, 1990-2004Parlier

Meteorological Type (cluster number)

Page 19: Envair DRI Alpine Geophysics

19

Daily 8-Hour Peak Ozone, 1990-2004Arvin

Meteorological Type (cluster number)

Page 20: Envair DRI Alpine Geophysics

20

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

Page 21: Envair DRI Alpine Geophysics

21

Directional Differences

Page 22: Envair DRI Alpine Geophysics

22

Directional Differences

Page 23: Envair DRI Alpine Geophysics

23

Directional Differences

Page 24: Envair DRI Alpine Geophysics

24

Directional Differences

Page 25: Envair DRI Alpine Geophysics

25

Mean Directional Differences

Page 26: Envair DRI Alpine Geophysics

26

850 mb Directional Differences

Page 27: Envair DRI Alpine Geophysics

27

Directional Differences

Page 28: Envair DRI Alpine Geophysics

28

Main Finding of Cluster Analysis

Clusters exhibit differences in transportdirections or distances. The differencesare more pronounced at some sites than others.

Page 29: Envair DRI Alpine Geophysics

29

Can Clusters Be Improved?

Maybe -

Direct comparisons of met types (clusters) to groupings determined from wind speed and direction at eachsite suggest room for improvement.

Page 30: Envair DRI Alpine Geophysics

30

Calm<1m/s

NE1-2m/s

SE1-2m/s

SW1-2m/s

NW1-2m/s

NE>2m/s

SE>2m/s

SW>2m/s

NW>2m/s

Chabot

83 8 1 12 34 3 2 5

6 41 12

12 64 109 44 55

4 7 4 16

1 3

16 5

1 5

1 2 21 4

36 24 20 1 3 5

1 42 10

1 4 2 10 11 1 4

1 4 2 8

1

2

3

4

5

6

7

8

9

10

11

12

Direction/Windspeed

Clu

ster

2

100

62 5

31 126

2

166 23

Page 31: Envair DRI Alpine Geophysics

31

Sacramento

212 1 13 27 41 6 1

5 157

148 26 207 19 14 131

16 1 10 7 25

22 16 286

6 5 59 30 319

1 3 18 233

20 5 85 23 7 82 12

24 9 55 1 99

7 4 9 1 5 69 2

1 62

2 1 38

1

3

4

5

6

7

8

9

10

11

12

Direction/Windspeed

Clu

ster

Calm<1m/s

NE1-2m/s

SE1-2m/s

SW1-2m/s

NW1-2m/s

NE>2m/s

SE>2m/s

NW>2m/s

32 5

12

SW>2m/s

21

Page 32: Envair DRI Alpine Geophysics

32

Fresno

290 3 1

1 2 4 71 59

346 1 2 2 186 5

38 1 15 5 13 3

79 2 7 196

25 1 1 226 1 159

3 18 2 231

2 30 198

77 1 1 90 15

3 1 12 79

39 1 13 6

1 40

1

3

4

5

6

7

8

9

10

11

12

Direction/Windspeed

Clu

ster

Calm<1m/s

NE1-2m/s

SE1-2m/s

SW1-2m/s

NW1-2m/s

NE>2m/s

SE>2m/s

SW>2m/s

NW>2m/s

302

6

3

50

Page 33: Envair DRI Alpine Geophysics

33

Preliminary Trends Assessment

Page 34: Envair DRI Alpine Geophysics

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

Page 35: Envair DRI Alpine Geophysics

35

Do trends differ among clusters?

Page 36: Envair DRI Alpine Geophysics

36

CO Trends

Page 37: Envair DRI Alpine Geophysics

37

Daily Morning CO – All Sites

Page 38: Envair DRI Alpine Geophysics

38

Fremont

-140

-120

-100

-80

-60

-40

-20

0

20

40

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Mo

rnin

g C

O (

pp

bv/

year

)

Error bars = 2 SE of slope

Page 39: Envair DRI Alpine Geophysics

39

Sacramento - T St.

-140

-120

-100

-80

-60

-40

-20

0

20

40

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Mo

rnin

g C

O (

pp

bv/

year

)

Error bars = 2 SE of slope

Page 40: Envair DRI Alpine Geophysics

40

Fresno - Drummond

-140

-120

-100

-80

-60

-40

-20

0

20

40

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Mo

rnin

g C

O (

pp

bv/

year

)

Error bars = 2 SE of slope

Page 41: Envair DRI Alpine Geophysics

41

Bakersfield

-140

-120

-100

-80

-60

-40

-20

0

20

40

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Mo

rnin

g C

O (

pp

bv/

year

)

Error bars = 2 SE of slope

Page 42: Envair DRI Alpine Geophysics

42

Sacramento and Northern Sierra Foothills - Cluster 1

-120

-100

-80

-60

-40

-20

0

20

40

60

80

Sacramento-TStreet

Elk Grove-Bruceville

Road

NorthHighlands-

Blackfoot Way

Sacramento-Del Paso

Manor

Roseville-NSunrise Blvd

Folsom-Natoma Street

Auburn-Dewitt-CAvenue

Grass Valley-Litton Building

Placerville-Gold Nugget

Way

Mo

rnin

g C

O (

pp

bv/

year

)

Error bars = 2 SE of slope

Page 43: Envair DRI Alpine Geophysics

43

Sacramento and Northern Sierra Foothills - Cluster 3

-120

-100

-80

-60

-40

-20

0

20

40

60

80

Sacramento-TStreet

Elk Grove-Bruceville

Road

NorthHighlands-

Blackfoot Way

Sacramento-Del Paso

Manor

Roseville-NSunrise Blvd

Folsom-Natoma Street

Auburn-Dewitt-CAvenue

Grass Valley-Litton Building

Placerville-Gold Nugget

Way

Mo

rnin

g C

O (

pp

bv/

year

)

Error bars = 2 SE of slope

Page 44: Envair DRI Alpine Geophysics

44

Sacramento and Northern Sierra Foothills - Cluster 5

-120

-100

-80

-60

-40

-20

0

20

40

60

80

Sacramento-TStreet

Elk Grove-Bruceville

Road

NorthHighlands-

Blackfoot Way

Sacramento-Del Paso

Manor

Roseville-NSunrise Blvd

Folsom-Natoma Street

Auburn-Dewitt-CAvenue

Grass Valley-Litton Building

Placerville-Gold Nugget

Way

Mo

rnin

g C

O (

pp

bv/

year

)

Error bars = 2 SE of slope

Page 45: Envair DRI Alpine Geophysics

45

Sacramento and Northern Sierra Foothills - Cluster 6

-120

-100

-80

-60

-40

-20

0

20

40

60

80

Sacramento-TStreet

Elk Grove-Bruceville

Road

NorthHighlands-

Blackfoot Way

Sacramento-Del Paso

Manor

Roseville-NSunrise Blvd

Folsom-Natoma Street

Auburn-Dewitt-CAvenue

Grass Valley-Litton Building

Placerville-Gold Nugget

Way

Mo

rnin

g C

O (

pp

bv/

year

)

Error bars = 2 SE of slope

Page 46: Envair DRI Alpine Geophysics

46

Sacramento and Northern Sierra Foothills - Cluster 9

-120

-100

-80

-60

-40

-20

0

20

40

60

80

Sacramento-TStreet

Elk Grove-Bruceville Road

NorthHighlands-

Blackfoot Way

Sacramento-DelPaso Manor

Roseville-NSunrise Blvd

Folsom-NatomaStreet

Auburn-Dewitt-CAvenue

Placerville-GoldNugget Way

Mo

rnin

g C

O (

pp

bv/

year

)

Error bars = 2 SE of slope

Page 47: Envair DRI Alpine Geophysics

47

NOx Trends

Page 48: Envair DRI Alpine Geophysics

48

Daily Morning NOx – All Sites

Page 49: Envair DRI Alpine Geophysics

49

Fremont

-10

-8

-6

-4

-2

0

2

4

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Mo

rnin

g N

Ox

(pp

bv/

year

)

Error bars = 2 SE of slope

Page 50: Envair DRI Alpine Geophysics

50

Sacramento - T St.

-10

-8

-6

-4

-2

0

2

4

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Mo

rnin

g N

Ox

(pp

bv/

year

)

Error bars = 2 SE of slope

Page 51: Envair DRI Alpine Geophysics

51

Fresno - Drummond

-10

-8

-6

-4

-2

0

2

4

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Mo

rnin

g N

Ox

(pp

bv/

year

)

Error bars = 2 SE of slope

Page 52: Envair DRI Alpine Geophysics

52

Bakersfield

-10

-8

-6

-4

-2

0

2

4

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Mo

rnin

g N

Ox

(pp

bv/

year

)

Error bars = 2 SE of slope

Page 53: Envair DRI Alpine Geophysics

53

Ozone Trends

Page 54: Envair DRI Alpine Geophysics

54

Daily Peak 8-Hour Ozone – All Sites

Page 55: Envair DRI Alpine Geophysics

55

Livermore

-2

-1.5

-1

-0.5

0

0.5

1

1.5

2

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Pea

k 8-

ho

ur

Ozo

ne

(pp

bv/

year

)

Error bars = 2 SE of slope

Page 56: Envair DRI Alpine Geophysics

56

Folsom

-2

-1.5

-1

-0.5

0

0.5

1

1.5

2

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Pea

k 8-

ho

ur

Ozo

ne

(pp

bv/

year

)

Error bars = 2 SE of slope

Page 57: Envair DRI Alpine Geophysics

57

Parlier

-2

-1.5

-1

-0.5

0

0.5

1

1.5

2

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Pea

k 8-

ho

ur

Ozo

ne

(pp

bv/

year

)

Error bars = 2 SE of slope

Page 58: Envair DRI Alpine Geophysics

58

Arvin

-2

-1.5

-1

-0.5

0

0.5

1

1.5

2

Cluster 1 Cluster 2 Cluster 3 Cluster 5 Cluster 6 Cluster 7 Cluster 8 Cluster 9 Cluster 11

Pea

k 8-

ho

ur

Ozo

ne

(pp

bv/

year

)

Error bars = 2 SE of slope

Page 59: Envair DRI Alpine Geophysics

59

What Have We Learned So Far?

Met clusters ~30 – 40% of ozone variability Clusters exhibit differences in mean transport

directions and distances. Might be able to improve distinctions among clusters.

Trends vary among clusters & sites Hypothesis: variations of ambient trends are a

function of spatial variations of emission trends

Page 60: Envair DRI Alpine Geophysics

60

Next Steps –

Compare ambient to emission trends – county level or groups of counties

Draft Phase I report & Phase II plan – July 1 Task 4 meeting – ? Final Phase I report & Phase II plan If Phase II approved, compare ambient trends to

emission trends occurring in the upwind areas of influence (need to grid emission estimates)