The long-range, cross-tropopause transport of COImpact by Region (fvgcm 1994-1996 SSTs) ⇒1994-1996...
Transcript of The long-range, cross-tropopause transport of COImpact by Region (fvgcm 1994-1996 SSTs) ⇒1994-1996...
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Bryan Duncan*, Susan Strahan*, Jose Rodriguez, Anne Douglass, Mark Schoeberl
NASA Goddard Space Flight Center *Goddard Earth Science & Technology (GEST) Center, UMBC
Nathaniel Livesey + MLS CO TeamJet Propulsion Laboratory
A Global Modeling Initiative (GMI) Study:The long-range, cross-tropopause transport of CO
GMI Meeting, Greenbelt, October 2006
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Schoeberl et al. [2006]
Inspiration ⇒ CO “Tape Recorder” in Aura MLS
Driven by Seasonal Biomass Burning and Convection.
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Southern Hemisphere by Region
Globe
CO Tape Recorder Driven by Seasonal Biomass Burning
Tg
CO
⇒ Fires set to clear agricultural fields/pastures before seasonal rains.
⇒ Seasonal convection lofts pollution to the upper troposphere.
Monthly Biomass Burning Emissions
Month
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But, why should anyone care about the CO tape recorder?
Biomass burning isn’t a source of key players in the stratosphere, right?
Because the pollutants may impact:
• Lifetimes of Trace Gases in Tropical Tropopause Layer (TTL)*
CO, NMHC, etc. + OH *Air in TTL resides several weeks before crossing the tropopause.
• Radiation Budget – Dynamics in TTLozone and aerosols - troposphere-to-stratosphere (TST) exchange
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Munich-Tokyo-12July
20
60
100
140
180
220
300 850 1400 1950 2500 3050 3600C
O(p
pbv)
mozaicGMI
Paris-Delhi-Jul11
20
60
100
140
180
150 450 750 1050 1350 1650
CO
(ppb
v)
MOZAICGMI
Model Comparison to MOZAIC Aircraft Data in Upper TroposphereCruise Altitude: 9-12 km
Japan Airlines Data
W. Pacific 40-130 ppbv1997 Indonesia <400 ppbv
Matsueda et al. [1998,1999]
MOZAIC Aircraft Data
Europe 50-140 ppbvAsia <150 ppbvBoreal BB >500 ppbv
Nedelec et al. [2005]
*Joanna to show more!
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215 hPa : September 21, 2005
Note: DAS fields = excessive tropical convection : MLS has water vapor issues.
Longitude
BB pollutionlofted to UT
Preliminary Version 2
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146 hPa : September 21, 2005
Height of convection too low? Averaging kernals?
Longitude
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⇒ Summary of MLS CO vs GMI CO Comparison
• Spatial distributions of MLS CO similar to model, though biased high.
• But only few days of data so far.
• Both model and observational limitations.
⇒ Application of MLS CO Data in UT/LS
• Transport of BB pollution to/in UT/LS
• BB causes much of the variation in CO in UT/LS
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Indonesian Fires 1997: CO Perturbation (%) ~200 mb
NOV
OCT
SEP
AUG
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⇒Troposphere-to-Stratosphere Exchange (TST) via Quasi-horizontal, Quasi-isentropic Exchange
⇒ But, pollution in Lowermost Stratosphere (LMS) returns totroposphere eventually
October 1997 : CO Perturbation (%)180° Longitude
Yellow Lines = Isentropes Red Line = Approximate TropopauseLatitude
Pres
sure
(mb)
LMS
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November 1997: CO Perturbation (%)
~100 mb – Near Tropical Tropopause
~80 mb – Lower Stratosphere
~ Tropical Tropopause
⇒ TST via Slow Ascent in TTLLa
titud
e
Longitude
Latit
ude
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October 1997: OH Perturbation (%)Global Zonal Mean
Pres
sure
(mb)
Latitude
Zonal Mean over Indian Ocean
Pres
sure
(mb)
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October 1997: Ozone Perturbation (ppbv)
Global Zonal Mean
Latitude
Zonal Mean over Indian OceanLocally: 25-100% increase over Maritime Continent!
Pres
sure
(mb)
Pres
sure
(mb)
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Impact by Region (fvgcm 1994-1996 SSTs)
⇒1994-1996 : weak ENSO phases
⇒ Climatological BB Emissions (Tg CO/y)southern Africa = 86northern Africa = 87South America = 60Southeast Asia = 82
⇒ These two pathways common for more typical burning events too.
⇒ Plumes of S. America and southern Africa mingle, though plumefrom S. America has bigger impact on [CO] in UT/LS due to deeper convection.
⇒ ENSO Effects*IndonesiaCentral America & Mexico
*IAV in emissions dominates over IAV of transport.
⇒IAV transport mainly due to IAV of convection (<30%).
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Conclusions• CO Comparison: MLS & GMI Combo
⇒ Very encouraging.⇒ Can we see evidence of biomass burning transport in UT?
• Only a few days of data.• Vertical resolution adequate?
• Big tropical burning event:⇒ TST of pollution via:
• slow ascent in TTL.• exchange in subtropical jets.
⇒ Impact on trace gases in TTL substantial.• Did pollution impact dynamics of TTL?
Aerosols: shortwave radiative forcing at surface = -10 W/m2
over Indian Ocean and -150 W/m2 over Indonesia! (Need to calculate heating rates!)
⇒ Driven by El Niño-induced drought & human activities.∴ 1997 scenario likely to repeat in future.
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Unresolved Issues• 2004-2005 Aura Period Emissions
⇒ Fossil Fuel – E. Asia 2003, but Rest of World?⇒ Biomass Burning – GFED2⇒ Biofuels ?⇒ Lightning Emissions
• Too Low Tropospheric CO
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Surface COCombo (1994) vs GMD (1992-1996)
Model is biased low when long-rangetransport is important globally.
Model generally has no bias whenphotochemical production isdominant.
Methylchloroform lifetime reasonable6.1 y (6.7 / 5.7 y in SH / NH)
Emissions?
*Accounts for missing NMHC.
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Southern Hemisphere by Region
Northern Hemisphere by Region
Month
Biomass Burning by RegionT
g C
O/m
onth