Use of Air Quality Forecasting as a Diagnostic Tool over the Northeastern US

19
Forecasting as a Diagnostic Tool over the Northeastern US Prakash Doraiswamy 1,* , Christian Hogrefe 1,2 , Winston Hao 2 , Kevin Civerolo 2 , J.-Y. Ku 2 , Robert Henry 2 and Gopal Sistla 2 1 Atmospheric Sciences Research Center, University at Albany, Albany, NY 2 Bureau of Air Quality Analysis and Research (BAQAR), New York State Department of Environmental Conservation (NYSDEC), Albany, NY * On assignment to BAQAR, NYSDEC CMAS Conference, Chapel Hill, NC Oct 1-3, 2007

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Use of Air Quality Forecasting as a Diagnostic Tool over the Northeastern US. Prakash Doraiswamy 1,* , Christian Hogrefe 1,2 , Winston Hao 2 , Kevin Civerolo 2 , J.-Y. Ku 2 , Robert Henry 2 and Gopal Sistla 2 1 Atmospheric Sciences Research Center, University at Albany, Albany, NY - PowerPoint PPT Presentation

Transcript of Use of Air Quality Forecasting as a Diagnostic Tool over the Northeastern US

Page 1: Use of Air Quality Forecasting as a Diagnostic Tool over the Northeastern US

Use of Air Quality Forecasting as a

Diagnostic Tool over the Northeastern US

Prakash Doraiswamy1,*, Christian Hogrefe1,2, Winston Hao2, Kevin Civerolo2,

J.-Y. Ku2, Robert Henry2 and Gopal Sistla2

1Atmospheric Sciences Research Center, University at Albany, Albany, NY2Bureau of Air Quality Analysis and Research (BAQAR), New York State

Department of Environmental Conservation (NYSDEC), Albany, NY*On assignment to BAQAR, NYSDEC

CMAS Conference, Chapel Hill, NCOct 1-3, 2007

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Outline Introduction about model-based air quality

forecasting An example – Evaluation of isoprene

predictions on a diurnal scale Diagnostic Analyses Results Conclusions

Page 3: Use of Air Quality Forecasting as a Diagnostic Tool over the Northeastern US

Introduction The Bureau of Air Quality Analysis and Research (BAQAR)

within the Division of Air Resources at New York State Department of Environmental Conservation (NYSDEC) has been performing air quality forecast over the Northeast US using CMAQ at 12 km grid resolution since June 2005.

Model inputs and outputs of these simulations have been (and continue to be) archived.

The overall objective is to assess the utility of the forecast-based simulations as a diagnostic tool by using a combination of analyses on the response of the model to biogenic, anthropogenic and secondary species.

To this end, we chose to evaluate the isoprene predictions, along with other supporting species, on a diurnal scale between June-August 2005.

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Short Overview of NYSDEC Forecast System Follows the air quality forecast system used by

EPA/NOAA. For the summer 2005 simulations, it consisted of

the ETA meteorological model, the PREMAQ emissions and meteorological preprocessor and the CMAQ (v4.4) model.

Each CMAQ simulation was performed for 48 hours starting at 12:00 noon Greenwich Mean Time (GMT).

Simulations initialized using default initial conditions (IC) on June 1, 2005. Everyday thereafter used modeled concentration fields from the previous day as IC.

Time-invariant boundary conditions were used.

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Approach Modeled isoprene concentrations from the CONC file for layer

1 (~35m thick) for June-Aug of 2005 were used in the analysis.

Measured concentrations were obtained from the EPA Air Quality System (AQS) for sites in the Northeastern US (ME, VT, NH, NY, MA, CT, RI, PA, NJ, MD, DE and DC).

Hourly concentrations of ethylene (anthropogenic and biogenic origin), ozone (product of photochemical reaction) and nitrogen dioxide (anthropogenic and chemical production) were also obtained, where available, for the same sites, to serve as supplemental information in the evaluation of model performance.

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Analysis Utilized data from June 12-August 31, 2005 in

the analyses, with June 1-11 as spin-up period to avoid effect of IC.

Compared hourly model predictions with measured concentrations.

Estimated correlation, normalized mean gross error and normalized mean bias for the entire summer period.

Examined diurnal profiles averaged over the entire summer period.

Reran the simulations for the same period using process analysis to confirm initial hypothesis.

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Model Performance for Isoprene over the Summer Period (June 12-August 31, 2005)

Site IDNo.of Pairs

Obs.Mean (ppb)

Pred.Mean (ppb)

Correlation, r

RMSEa

(ppb)No.of Pairs,

where Obs.> 0NMGEb

(%) NMBc (%)

090019003 1616 0.477 0.231 0.446 0.718 1334 75.7 -53.1090031003 1729 0.495 0.263 0.433 0.589 1714 73.8 -46.9090090027 1865 0.260 0.284 0.525 0.433 1691 82.6 7.7110010043 1520 0.402 0.959 0.404 1.210 1348 165.3 128.4230052003 1831 0.183 0.219 0.255 0.516 1113 102.9 -11.6230090102 1630 0.311 0.106 0.318 0.420 1337 81.2 -67.4230313002 1602 0.435 0.383 0.441 0.644 1437 76.1 -13.2240053001 803 0.429 0.524 0.544 0.575 794 75.1 22.0250092006 1454 1.001 0.468 0.418 1.158 1428 72.1 -53.3250094004 1606 0.491 0.196 0.351 0.805 1501 85.6 -60.2250130008 1625 0.818 0.446 0.393 0.917 1615 71.5 -45.5250154002 824 1.989 0.526 0.380 2.943 820 79.3 -73.6330111011 1515 0.885 0.765 0.580 1.022 1504 63.8 -13.9340070003 1810 0.397 1.180 0.524 1.323 1803 214.3 196.9340210005 1796 0.439 0.697 0.502 0.716 1783 102.8 58.4340230011 1583 0.783 1.141 0.542 1.236 1575 88.4 45.3360050083 1526 0.769 0.300 0.272 0.922 1525 78.2 -61.0420010001 1722 0.479 1.370 0.634 1.995 1644 211.2 185.2

a RMSE: Root Mean Square Error =

2

1

1

n

iobspred CC

n

b NMGE: Normalized Mean Gross Error =

obs

obspred

Cn

CCABSn

1

1*100

c NMB: Normalized Mean Bias =

obs

obspred

Cn

CCn1

1*100

CT

D.C

ME

MD

MA

NH

NJ

NYPA

State

59% data missing

58% data missing

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Distribution of Daily Correlations by Site (Isoprene) Correlation between

predicted and measured hourly isoprene concentrations each day.

Only days with 18 hours or more of valid pairs of data were included (i.e., at the least, 75% data availability each day) .

Median daily correlations ranged from 0.24 to 0.72

-1.0-0.8-0.6-0.4-0.20.00.20.40.60.81.0

SI:0

90019003

SI:0

90031003

SI:0

90090027

SI:11

0010043

SI:2

30052003

SI:2

30090102

SI:2

30313002

SI:2

40053001

SI:2

50092006

SI:2

50094004

SI:2

50130008

SI:2

50154002

SI:3

30111

011

SI:3

40070003

SI:3

40210005

SI:3

40230011

SI:3

60050083

SI:4

20010001

Site

Corr

ela

tion

Corr

ela

tion,

r

Site

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Hourly Bias of Isoprene (Predicted – Measured) at Selected Sites

-6.0-5.0-4.0-3.0-2.0-1.00.01.02.03.04.05.06.0

0 1 2 3 4 5 6 7 8 9 10

11 12

13

14

15

16

17

18

19

20

21

22

23

Hour

Hourly

Bia

s

-6.0-5.0-4.0-3.0-2.0-1.00.01.02.03.04.05.06.0

0 1 2 3 4 5 6 7 8 9 10

11 12

13

14

15

16

17

18

19

20

21

22

23

Hour

Hourly

Bia

s

-20.0-16.0-12.0-8.0-4.00.04.08.0

12.016.020.0

0 1 2 3 4 5 6 7 8 9 10

11 12

13

14

15

16

17

18

19

20

21

22

23

Hour

Hourly

Bia

s

Site 360050083

New York Botanical Gardens (NYBG)

Urban

Site 340210005

New Jersey, Riders College (NJRC)

Suburban

Site 420010001

Pennsylvania NARSTO Site at Arendtsville (PANARSTO)

Rural

Hourl

y B

ias

(ppb)

Hour

0

0.2

0.4

0.6

0.8

1

1.2

1.4

1.6

1.8

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Iso

pre

ne

Co

nc.

(pp

b)

Obs. Isoprene (ppb) CMAQ-pred. Isoprene (ppb)

00.20.40.60.8

11.21.41.61.8

2

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Iso

pre

ne

Co

nc.

(pp

b)

0

1

2

3

4

5

6

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Iso

pre

ne

Co

nc.

(pp

b)

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Questions of Interest Why do we see dual peak in predicted concentrations

when the measurements do not show such a pattern ? What are the reasons for agreement/ disagreement

between measurements and predictions? The potential solution lies in examining possible sources

and sinks Sources: Biogenic sources, addition of isoprene by

convection/advection from adjacent cells Sinks: Consumption by reaction; Depletion by

convection/advection to adjacent cells; Currently in CMAQ, dry deposition is not a sink for isoprene.

The dual peak could be interpreted as a “depression” during the mid-day hours.

In CMAQ-CB4, consumption of isoprene is through a set of 5 reactions

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Reactions Consuming IsopreneRx#

Reac. 1

Reac. 2

ISPD FORM XO2 HO2 PAR OH Others Rate Const.(mol/cc)-2sec-1

75 ISOP O 0.75 0.5 0.25 0.25 0.25 --- 0.25C2O3 3.6E-11

76 ISOP OH 0.912 0.629 0.991 0.912 --- --- 0.088 XO2N

2.54E-11 * exp(407.6/T)

[9.97E-11] @ 25 °C

77 ISOP O3 0.65 0.6 0.2 0.066 0.35 0.266 0.15ALD2 + 0.066CO + 0.2C2O3

7.86E-15 * exp(-1912/T)

[1.29E-17] @ 25 °C

78 ISOP NO3 0.2 --- 1 0.8 2.4 --- 0.8 NTR + 0.2NO2 + 0.8ALD2

3.03E-12 * exp(-448/T)

[6.74E-13] @ 25 °C

94 ISOP NO2 0.2 --- 1 0.8 2.4 --- 0.8 NTR + 0.2NO + 0.8ALD2

1.49E-19

R76 typically dominates during day time; R78 dominates @ night time

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0

0.5

1

1.5

2

2.5

3

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Iso

pre

ne

Co

nc.

(pp

b)

-100-90-80-70-60-50-40-30-20-1001020304050607080

NO

2 (p

pb

), H

O2

(pp

t)

Obs. NO2 (ppb) Obs. Isoprene (ppb)CMAQ-pred. Isoprene (ppb) CMAQ-pred. HO2 (ppt)CMAQ-pred. NO2 (ppb)

0

10

20

30

40

50

60

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Ozo

ne

Co

nc

. (p

pb

)

0

200

400

600

800

1000

1200

1400

1600

1800

2000

PB

L H

eig

ht

(m)

Obs. O3 (ppb) CMAQ-pred. O3 (ppb) PBL Height (m)

0

0.2

0.4

0.6

0.8

1

1.2

1.4

1.6

1.8

2

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Ob

ser

ved

Eth

ylen

e C

on

c.

(pp

b)

0

0.5

1

1.5

2

2.5

3

3.5

4

4.5

CM

AQ

Pre

dic

ted

Eth

yle

ne

Co

nc.

(p

pb

)

Obs. Ethylene (ppb) CMAQ-pred. Ethylene (ppb)

NYBG (360050083),

Urban NO2 concentrations over-

predicted Consistent with predicted

night-time O3 being lower than observed (due to scavenging by NOx).

PBL height seems reasonable for summer

Ethylene, while over-predicted, appears to track measured profile

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NJRC (340210005),

Suburban Predicted Isoprene tracks

measured profiles Isoprene emissions

appear to be overestimated

0

0.5

1

1.5

2

2.5

3

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Iso

pre

ne

Co

nc.

(pp

b)

-70

-60

-50

-40

-30

-20

-10

0

10

20

30

NO

2 (p

pb

), H

O2

(pp

t)

Obs. NO2 (ppb) Obs. Isoprene (ppb) CMAQ-pred. Isoprene (ppb)

CMAQ-pred. HO2 (ppt) CMAQ-pred. NO2 (ppb)

0

10

20

30

40

50

60

70

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Ozo

ne

Co

nc.

(p

pb

)

0

200

400

600

800

1000

1200

1400

1600

1800

2000

PB

L H

eig

ht

(m)

Obs. O3 (ppb) CMAQ-pred. O3 (ppb) PBL Height (m)

0

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Ob

ser

ved

Eth

ylen

e C

on

c. (

pp

b)

0

0.5

1

1.5

2

2.5

CM

AQ

Pre

dic

ted

Eth

ylen

e C

on

c. (

pp

b)

Obs. Ethylene (ppb) CMAQ-pred. Ethylene (ppb)

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PANARSTO (420010001),

Rural

Predicted Isoprene tracks measured profiles

Isoprene emissions appear to be overestimated

0

1

2

3

4

5

6

7

8

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Iso

pre

ne

Co

nc.

(pp

b)

-100-90-80-70-60-50-40-30-20-1001020304050

NO

2 (p

pb

), H

O2

(pp

t)

Obs. NO2 (ppb) Obs. Isoprene (ppb) CMAQ-pred. Isoprene (ppb)

CMAQ-pred. HO2 (ppt) CMAQ-pred. NO2 (ppb)

0

10

20

30

40

50

60

70

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Ozo

ne

Co

nc

. (p

pb

)

0

200

400

600

800

1000

1200

1400

1600

1800

2000

PB

L H

eig

ht

(m)

Obs. O3 (ppb) CMAQ-pred. O3 (ppb) PBL Height (m)

0

0.05

0.1

0.15

0.2

0.25

0.3

0.35

0.4

0.45

0.5

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Ob

ser

ved

Eth

ylen

e C

on

c.

(pp

b)

0

0.2

0.4

0.6

0.8

1

1.2

CM

AQ

Pre

dic

ted

Eth

yle

ne

Co

nc.

(p

pb

)

Obs. Ethylene (ppb) CMAQ-pred. Ethylene (ppb)

Page 15: Use of Air Quality Forecasting as a Diagnostic Tool over the Northeastern US

What does Process Analysis

show ? For surface layer, emission is

major source; vertical diffusion and chemistry are the dominant loss processes.

For upper layers (not shown), chemistry is the dominant loss process

-8

-6

-4

-2

0

2

4

6

8

0 2 4 6 8 10 12 14 16 18 20 22

Hour

Iso

pre

ne

Co

nc.

(p

pb

/hr)

NYBG

-25

-20

-15

-10

-5

0

5

10

15

20

25

0 2 4 6 8

10 12 14 16 18 20 22

Hour

Iso

pre

ne

Co

nc.

(p

pb

/hr)

NJRC

-25

-20

-15

-10

-5

0

5

10

15

20

25

0 2 4 6 8

10 12 14 16 18 20 22

Hour

Iso

pre

ne

Co

nc

. (p

pb

/hr)

Emission

Horizontal Advection

Vertical Advection

Clouds

Chemistry

Dry Deposition

Vertical Diffusion

Horizontal Diffusion

CMAQv46 Isoprene(ppb)CMAQv44 Isoprene(ppb)Obs. Isoprene (ppb)

PANARSTO

Page 16: Use of Air Quality Forecasting as a Diagnostic Tool over the Northeastern US

Day time profile At NYBG, over-prediction of isoprene loss during mid-day

hours could be mostly explained by chemical reactions (~0.5 ppb/hr), probably due to overestimation of NOx. However, it is also quite possible that the model is underestimating additional sources (emissions, mixing from above?)

For NJRC and PANARSTO, the process analysis confirmed emissions to be the major source. Mixing processes are likely modeled satisfactorily, given the similarity of observed vs. predicted profiles of isoprene, ozone and ethylene at these two sites. It is likely emissions are overestimated resulting in a positive bias.

Page 17: Use of Air Quality Forecasting as a Diagnostic Tool over the Northeastern US

Evening/Night time peak? Evening peak was present at all three sites (8-9 pm at NYBG, 6 pm

at other two sites). While horizontal advection from adjacent cells contributed to some

addition, it was not a major source. Night-time isoprene loss is subject of extensive research

Reaction of ISOP + NO3 (Starn et al., 1998) Vertical diffusion (Sillman et al, 2002; Hurst et al., 2001) Reaction with OH (Hurst et al., 2001) Other unknown (as yet) mechanisms (Goldan et al., 1995)

Starn et al. (1998) observed that rapid isoprene loss was associated with conditions when [O3]*[NO2] > 300 ppb2. At NYBG, while observed conditions fall in this range (dropped from 657 to 382 ppb2, suggesting the possibility of loss by ISOP + NO3 rxn), CMAQ predictions showed < 200 ppb2 (supporting the argument that NO emissions were overestimated)

Cause of peak at other two sites is not clear at this time.

Page 18: Use of Air Quality Forecasting as a Diagnostic Tool over the Northeastern US

Conclusions Archived forecast simulations presents a unique

opportunity to evaluate the model under varied atmospheric conditions. While this specific example could have also been done using retrospective modeling, the presence of archived simulations allows us to look at other seasons/years of interest.

Overall, the model appeared to track diurnal profile at most sites.

Analysis revealed that the causes of model performance differ by site. Possible overestimation of NOx emissions at NYBG Possible overestimation of isoprene emissions at NJRC and

PANARSTO

Page 19: Use of Air Quality Forecasting as a Diagnostic Tool over the Northeastern US

References Goldan, P. D., W. C. Kuster, F. C. Fehsenfeld and S. A. Montzka (1995). "Hydrocarbon measurements

in the southern United States: The Rural Oxidants in the Southern Environment (ROSE) Program 1990." Journal of Geophysical Research 100(25): 945-963.

Hurst, J. M., D. J. Barket, O. Herrera-Gomez, T. L. Couch, P. B. Shepson, I. Faloona, D. Tan, W. Brune, H. Westberg, B. Lamb, T. Biesenthal, V. Young, A. Goldstein, J. W. Munger, T. Thornberry and M. A. Carroll (2001). "Investigation of the nighttime decay of isoprene." Journal of Geophysical Research 106(D20): 24335-24346.

Sillman, S., M. A. Carroll, T. Thornberry, B. K. Lamb, H. Westberg, W. H. Brune, I. Faloona, D. Tan, P. B. Shepson, A. L. Sumner, D. R. Hastie, C. M. Mihele, E. C. Apel, D. D. Riemer and R. G. Zika (2002). "Loss of isoprene and sources of nighttime OH radicals at a rural site in the United States: Results from photochemical models." Journal of Geophysical Research 107(D5).

Starn, T. K., P. B. Shepson, S. B. Bertman, D. D. Riemer, R. G. Zika and K. Olszyna (1998). "Nighttime isoprene chemistry at an urban-impacted forest site." Journal of Geophysical Research 103(D17): 22437-22448.