inverse modeling of co emissions results for biomass burning
DESCRIPTION
Multi-year inversion of CO sources using MOPITT data. Inverse Modeling of CO Emissions Results for Biomass Burning. Gabrielle Pétron National Center for Atmospheric Research [email protected]. Land clearing fires in the Kalimantan region of the island of Borneo, Indonesia NASA photo, 09/18/91. - PowerPoint PPT PresentationTRANSCRIPT
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
Inverse Modeling of CO Emissions
Results for Biomass Burning
Gabrielle Pétron
National Center for Atmospheric [email protected]
Multi-year inversion of CO sources using
MOPITT data
Land clearing fires in the Kalimantan region of the island of Borneo, Indonesia
NASA photo, 09/18/91
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
Role of CO in the troposphere Oxidation capacity of the atmosphere Precursor of tropospheric ozone Indoor and urban pollutant
Houston
Santiago
http://eces.org/archive/gallery/airgfx
NOx
CO2
+ HO2COV CONOx
+ NOCO + OH + O2
O3+UVNO2
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
CO emissions
Known : nature of sources combustion of C matter, chemical production...
Uncertain : sources quite variable (x,t) intensities location timing, seasonality, interannual variations splitting : fossil fuel/biofuel....
Tools to study CO budget: emissions inventories observations models
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
Sources & Sinks of CO
Fossil fuel : 300-600 Biomass burning: 300-900
(forests, savannas, agric. waste burning, fuel wood use)
Vegetation : 50-200 Oceans : 6- 30 Methane oxidation : 400-1000 HCNM oxidation : 300-1000
TOTAL Source = 1400 – 3700 TgCO/yr Photochemical sink : 1400-2600 Surface deposition: 150-500
TOTAL Sink = 1550 – 3100 TgCO/yr
TgCO/yr
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
Tools to study CO budget
Observations local,regional,global in situ/remote sensing continuous, campaign
Models city-scale,regional,global transport/chemistry (on/offline)
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
July 2000 Total column of CO : MOZART2 (top) and MOPITT (bottom)
JUL MOZART2, CO-column, scale=1.e17
-100 0 100 Longitude
-60
-40
-20
0
20
40
60
JUL MOPITT, CO-column, scale=1.e17
-100 0 100 Longitude
-60
-40
-20
0
20
40
60
underestimation of biomass burning emissions
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
Motivations for Inverse Modeling and Data Assimilation
Quality and expansion of the Observing Systems surface stations networks remote sensing intensive regional campaign
Progress in Modeling computation capacity representativeness of complex CTMs
o improved parameterizations – chemistry (more species, trace gases and particles)– transport (esp. analyzed meteorological fields)
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
MOPITT/MOZART CO at 850 hPaPhase 1 : April 2000 to April 2001
Phase 2 : September 2001 to December 2003
A priori biomass burning (WF) monthly emissions in MOZART: scaling of MODIS fire counts
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
Multi-year CO inversion
MOZART CTM MOPITT satellite data
April 2000-December 2003
A Priori Emission Inventory
Atmospheric CTM
MOPITT Observed COJUL MOZART2, CO-column, scale=1.e17
-100 0 100 Longitude
-60
-40
-20
0
20
40
60
JUL MOPITT, CO-column, scale=1.e17
-100 0 100 Longitude
-60
-40
-20
0
20
40
60
JUL MOZART2, CO-column, scale=1.e17
-100 0 100 Longitude
-60
-40
-20
0
20
40
60
JUL MOPITT, CO-column, scale=1.e17
-100 0 100 Longitude
-60
-40
-20
0
20
40
60
Optimized Emission Inventory
INVERSE MODELING
MOZART Modeled CO
North of 14oN
0
20
40
60
80
100
J0 M M J S N J1 M M J S N J2 M M J S N J3 M M J S N
Tg
CO
/mo
nth Fossil fuel Biofuel Wildland fires
North of 14oN
0
20
40
60
80
100
J0 M M J S N J1 M M J S N J2 M M J S N J3 M M J S N
Tg
CO
/mo
nth
POET CO emissions + a priori WF Optimized CO emissions
Figure 2 Figure 3
The discrepancies between the observed and the modeled CO
distributions can be used to optimize poorly known parameters of the model
– here, CO anthropogenic
emissions.
1
2 3
4
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
CO FF BF WF optimized
emissions for four latitudinal
bands
North of 14degN
0102030405060708090
100
J0 M M J S N J1 M M J S N J2 M M J S N J3 M M J S N
Tg
CO
/mo
nth
Fossil fuel Biofuel Wildland fires
Equator-14degN
0
10
20
30
40
50
60
J0 M M J S N J1 M M J S N J2 M M J S N J3 M M J S N
Tg
CO
/mo
nth
Equator-14degS
0
10
20
30
40
50
60
J0 M M J S N J1 M M J S N J2 M M J S N J3 M M J S N
Tg
CO
/mo
nth
South of 14degS
0
5
10
15
20
25
30
35
40
45
J0 M M J S N J1 M M J S N J2 M M J S N J3 M M J S N
Tg
CO
/mo
nth
Fossil Fuel Use
Biofuel Use
Wildland Fires
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
CO WF Emissions
Wildland fires PRIOR
0
50
100
150
200
250
Europ
eUSA
East A
sia
South
Asia
North
Asia
Canad
a
Ocean
ia
South
Eas
t Asia
North
Eq
Africa
South
Eq
Africa
South
Afri
ca
Centra
l Am
erica
South
Cen
t Am
erica
South
Am
erica
Tg
CO
/yr
2000 2001 2002 2003
Wildland fires POST
0
50
100
150
200
250
Europe
USA
East A
sia
South
Asia
North
Asia
Canada
Oce
ania
South
East
Asia
North
Eq
Africa
South
Eq A
frica
South
Afri
ca
Centra
l Am
erica
South
Cen
t Am
erica
South
Am
erica
Tg
CO
/yr
2000 2001 2002 2003
inversion results
a priori inventory based on MODIS fire counts
North Asia: high emissions in 2002 and 2003
South East Asia: high emissions in 2003
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
CO WF emissions in boreal regions
van der Werf (MODIS fc, CASA model,...)
Ito and Penner (GBA 2000,...): artifact ~no fire detection at high latitude
fire counts: sampling bias < polar orbit satellite only sees a fraction of the fires
yet useful to detect fires in dense tropical forest
burnt area: integrated fire activity over 10 days
problem for both approaches: what is the fraction of pixel burnt
emission factors: “large” uncertainties (flaming/smoldering, ...)
North Asia
0
5
10
15
20
25
30
J0 M M J S N J1 M M J S N J2 M M J S N J3 M M J S N
Tg
CO
/mo
nth
prioroptimizedvan der WerfIto and Penner
Canada/Alaska
0
2
4
6
8
10
12
J0 M M J S N J1 M M J S N J2 M M J S N J3 M M J S N
Tg
CO
/mo
nth
prior optimizedvan der Werf Ito and Penner
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
CO WF emissions in AfricaNorth Equatorial Africa
0
10
20
30
40
50
J0 M M J S N J1 M M J S N J2 M M J S N J3 M M J S N
Tg
CO
/mo
nth
prior optimized van der Werf Ito and Penner
South Equatorial Africa
0
5
10
15
20
25
J0 M M J S N J1 M M J S N J2 M M J S N J3 M M J S N
Tg
CO
/mo
nth
prior optimized van der Werf Ito and Penner
South Africa
0
5
10
15
20
25
30
J0 M M J S N J1 M M J S N J2 M M J S N J3 M M J S N
Tg
CO
/mo
nth
prior optimized van der Werf Ito and Penner
no inversion:
January to March 2000 & May to Aug 2001
>0o: fairly good a priori emissions
0-10oS: emissions do not decrease as fast as fire counts regional total
< 10oS : clear a priori under-estimation
27-28/10/2005 IGBP-QUEST Fire Fast Track Initiative Workshop
Conclusions
Inversion results: Results quite robust/ inversion parameters
(paper to be submitted) WF emissions are not proportional to fire
counts
Emission Modeling: Intercomparison with WF top-down inventoriesassess parameterization
Emission Inference: Requires to use several fire products AND
chemical data