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Spectroscopic Study of Atmospheric Trace Gases Using PARIS-IR from
Waterloo Atmospheric Observatory in 2005 and 2006
Dejian Fu, Kaley Walker, Keeyoon Sung, Chris Boone, Peter Bernath
Waterloo Atmospheric Observatory (WAO)
Goals of WAOTo observe the concentrations of atmospheric trace gases simultaneouslyTo conduct measurements over large time scales for observing trendsTo assist in validating Atmospheric Chemistry Experiment Fourier Transform Spectrometer (ACE-FTS)
Location of WAOThe rooftop of the Center for Environmental and Information Technology,
University of Waterloo (43.47º, 80.54ºW, 319 m above sea level) Main instruments at WAO
1. Portable Atmospheric Research Interferometric Spectrometer, for the Infrared (PARIS-IR)
2. ABB Bomem DA8 (MOPD = 50 cm, Near IR-Vis-UV) From PARIS-IR spectra, we have been able to retrieve 13 species: O3, HCl, CH4, N2O, H2O, HNO3, NO, NO2, CCl3F, CCl2F2, HF, CO, OCS
Portable Instrument - PARIS-IR
MANTRA 2004 balloon
campaign
mini-MANTRA campaign
WAO
ACE Arctic Validation Campaigns
Ground-based Observations of PARIS-IR
azimuth gimbal
sun sensor
pointing mirror
solar beam
Max. Res. : 0.02 cm-1
Meas. Reg.: 750 – 4400 cm-1 Max. Scan Speed: 2.5 cm/sDetectors : InSb and HgCdTe
elevation gimbal
GPS receiver
control computer
pendulum arm
ZnSe beam splitter
O3
N2O
CO2
CH4
HFHCl
CO2 H2O
HNO3
O3
NO
Spectra recorded on July 30th, 2005 at WAO
Retrievals: Process of Going from Spectra to Trace Gas Concentration
Computed Spectra
Observed Spectra
Optimal Estimation
a priori VMR profiles from TAO
p & T profile from NCEP and 1976 USA standard atmosphere
spectral line parameters (HITRAN2004)
air mass (RAYTRACE)
altitude grid (29 layers)
Discrepancy within a specified
convergence criterion
Output retrieval result
Volume Mixing Ratio (VMR)National Centers for Environment Prediction (NCEP)Toronto Atmospheric Observatory (TAO)
Adjust VMR Profile
yes
No
A retrieval code named SFIT2 (C. Rinsland et al). used for trace gas retrievals. It contains a line-by-line calculation program for the forward model and uses the optimal estimation method for the inverse algorithm (C. Rodgers et al. ).
A Sample for CH4 Retrieval Using Spectrum Recorded on July 30, 2005
2859.3 2859.4 2859.5 2859.6 2859.7 2859.8 2859.9 2860 2860.1-4-2024
Res
idu
als(
%)
2859.3 2859.4 2859.5 2859.6 2859.7 2859.8 2859.9 2860 2860.10.4
0.5
0.6
0.7
0.8
0.9
1.0
1.1
(cm-1)
Am
plit
ud
e (a
rbit
ary
un
it)
Meas Spec.Calc. Spec.
Column Densities Retrieved from Spectra on July 30, 2005
Daily Mean Column3.58 X 1019 molecules/cm2
1 Standard Deviation3.51 X 1017 molecules/cm2
Error bars indicatetotal errors (systematic and random errors).
Each data point is obtained from 20 spectra recorded in 6.6 minutes.
Characterization of CH4 Retrieval
Degree of freedom =2.07
-0.2 0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.80
5
10
15
20
25
30
35
Averaging kernel values
Alt
itu
de
(km
)
12.5 - 100 km
0.31 - 12.5 km
total Column
CH4MW2835
Characterization of O3 Retrieval
-0.2 0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.80
5
10
15
20
25
30
35
40
45
50
Averaging kernel values
Alt
itu
de
(km
)
12.5 - 100 km
0.31 - 12.5 km
total Column
O3MW2775
Degree of freedom =1.02
Error Estimation
CH4 O3
MW2835 MW27752.5 2.7< 1 < 1< 1 < 12.8 3.02.0 5.01.3 4.36.2 8.96.6 11.17.2 11.5Total Error
Systematic Errors
Spectroscopic ParameterEmpirical Apodization Function
A prioriSubtotal
Error SourcesErrors (in %)
Random Errors
Retrieval ErrorSolar Zenith Angle
TemperatureSubtotal
Total Ozone from MSC Brewer UV Spectrometer at Toronto and PARIS-IR at WAO
05/01/01 05/04/01 05/07/01 05/10/01 06/01/01 06/04/01 06/07/01250
300
350
400
450
500
Date (YY/MM/DD)
To
tal O
zon
e (i
n D
U)
MSC Daily Total Ozone MSC Monthly Mean OzonePARIS-IR Daily Ozone
Map of ACE Occultation Location within 1000 km from June 2005 to May 2006
12 coincident ACE observations
Partial Column Densities of O3 from ACE and PARIS-IR (17.5 km to 100 km)
26/06/05 03/07/05 10/07/05 17/07/05 24/07/05 31/07/05200
210
220
230
240
250
260
270
280
290
300
Date
To
tal C
olu
mn
(in
DU
)
ACE-FTSACE-MAESTRO (UV)ACE-MAESTRO (Vis)PARIS-IR
Agree to within 5%
Partial Column Densities of HCl from ACE and PARIS-IR (17.5 km to 100 km)
26/06/05 03/07/05 10/07/05 17/07/05 24/07/05 31/07/052.4
2.5
2.6
2.7
2.8
2.9
3
3.1
3.2
3.3
3.4x 10
15
Date
To
tal C
olu
mn
(in
#/c
m2)
ACE-FTSPARIS-IR
Agree to within 5%
Partial Column Densities of HNO3 from ACE and PARIS-IR (17.5 km to 100 km)
26/06/05 03/07/05 10/07/05 17/07/05 24/07/05 31/07/056.5
7.0
7.5
8.0
8.5
9.0
Date
To
tal C
olu
mn
(in
#/c
m2)
ACE-FTSPARIS-IR
Differences between 2% and 12%
Summary and Future work
Completed 50 days observations were performed using PARIS–IR at WAO from
June 2005 to May 2006. 12 ACE occultations were recorded within 1000 km of WAO.
Column densities of 7 trace gases were retrieved using SFIT2 program.
Good agreement of the results are achieved between PARIS–IR, Brewer, and ACE-FTS, ACE-MAESTRO measurements.
To do Observations and further analysis are on going at WAO. Correlations between species will be investigated. Simultaneous atmospheric observations using PARIS-IR and DA8 at
WAO are in our plan.
Acknowledgements
World Ozone and Ultraviolet Radiation Data Center
Meteorological Service of Canada
Natural Sciences and Engineering Research Council, Canada
Canadian Space Agency