lamarque , solomon, portmann , deshler, hofmann, smith, liley , and trickl
DESCRIPTION
Anthropogenic influence on stratospheric aerosol changes through the Asian monsoon: observations, modeling and impact. Lamarque , Solomon, Portmann , Deshler, Hofmann, Smith, Liley , and Trickl. Background stratospheric aerosols and volcanic perturbations. Changes in the ‘background’? - PowerPoint PPT PresentationTRANSCRIPT
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Anthropogenic influence on stratospheric aerosol changes through the Asian monsoon:
observations, modeling and impact
Lamarque, Solomon, Portmann,
Deshler, Hofmann, Smith,Liley, and Trickl
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10-5
10-4
10-3
10-210-5
10-4
10-3
10-2
104
105
106
1970 1975 1980 1985 1990 1995 2000 2005
104
105
106
Hampton (37oN, 76oW), Garmisch (47oN, 11oE)
Inte
grat
ed B
acks
catt
er (
sr-1
)
Latitude
< 30o
> 30o
São José dos Campos (23oS, 46oW), Mauna Loa (20oN, 156oW)
20-25 km Laramie, Wyoming, (41oN, 105oW)
Latitude
< 30o
> 30o
15-20 km N(r > 0.15 m) N(r > 0.25 m))
5 km
Aer
osol
col
umn
(cm
-2)
Years
Background stratospheric aerosols and volcanic perturbations. Changes in the ‘background’?
Deshler, T. (2008), A Review of Global Stratospheric Aerosol: Measurements, Importance, Life Cycle, and Local Stratospheric Aerosol, Atmos. Res., 90, 223-232.
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Sources of the background sulfate layer?
Crutzen (1976): OCS
Chin and Davis, Weisenstein et al., Pitari, others: yes, but much more sulfur is needed.
Aircraft emissions?Surface SO2 emissions?Other?
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Hofmann et al., GRL, 2009
What is causing the increase in sulfate after the mid-1990s?
Coal burning in China?
But….how can this be when estimated total global sulfur emission has dropped….and AVHRR tropospheric optical depth isn’t going up globally……
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Compare Ground-Based and SAGE
Mauna LoaVsSAGE tropical mean
LaramieVs SAGEZonal mean
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Large aerosol volume and extinction changes are seen in the lowermost stratosphere in many independent datasets
3-7%/yr, up to 10%/yr in some places
1998-2004 SAGE trend – avoids possibly significant eruptions (Manam was in 2005)
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Large increases in aerosol are seen at various SAGE wavelengths from 1998-2004, and are confined to lower stratosphere
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Emissions
Sulfate in upper trop
Sulfate in lower strat; special role of monsoon
Lamarque et al., 2009: examine issue using CAM (NCAR model); tropospheric sulfur emissions updated by Smith; sulfur chemistry by Barth/Rasch et al.
Considers emissions, transport, washout, etc. in troposphere
Computes mass entering stratosphere
See also Notholt et al., 2005
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The Asian Summer Monsoon is a Special Conduit to the Stratosphere
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Tropospheric air
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CAM Model Performance for CO Transport in the Asian Monsoon
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Niwano et al.:
Very strong seasonal cycle in stratospheric aerosol, high values in NH summer coming into stratosphere in tropics; deficit at the entry point in winter.
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Important fingerprints of the aerosol signal in season, altitude, latitude. Matches the expected pattern from the modeled coal emissions.
SAGE anomaly in July compared to annual mean
Model anomaly in July compared to annual mean
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SAGE anomalies by season
Model reproduces MAM, JJA, and SON well but does not get the maximum in DJF in the SH.
Model transport, esp from NH to SH?
Biomass burning?
S. American monsoon?
African monsoon?
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Good agreement between data and models in the NH…..some signal but too weak in SH
Change from 1998-2004Including all emissions
Change from 1998-2004Including all but China China contribution
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Surface chemistry plays key role in partitioning of NOx/NOy and ClO/Cly, very strong at LOW values of aerosol (and when wet!).
More aerosol gives more ClO and more ozone loss.
≈50% more aerosol mass in 2008 compared e.g. to 1998 -> 35% more aerosol surface area -> 0.5-1% ozone loss at 15-18 km, cf about 5% depletion obs there since 1975. Therefore, Chinese aerosols have impeded ozone recovery that would otherwise have occurred by about 10-20% at this level. Other altitudes? Biggest aerosol changes are in the lowermost stratosphere.
Future? Lower emissions likely in 2008 and 2009. Longer term?
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Concluding Remarks
• Evidence for changes in background stratospheric aerosol layer since the late-1990s, not attributable to volcanic eruptions, seen systematically in many different datasets. Hofmann et al. (2009) first to observe, ascribe to Chinese coal burning.• This study: importance of monsoon flow, see also Notholt et al. 2005 JGR re aerosols; also many papers on other constituents• Match between model and data fingerprints in altitude, latitude and season in the NH.• SH subtropics? Extratropics?• Suggests Chinese coal burning has made the chlorine in the stratosphere more effective for ozone loss, offsetting some of the gains that the Montreal Protocol would have achieved in the lower stratosphere in the past 10 years. Future? • Field experiments needed. Isotopic sulfur to derive SO2 source from coal?
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Factors affecting lidar seasonal signals?
Any column measurement will have a seasonalcycle, even an inert tracer
Also
Mauna Loa is a special case. This site is ‘tropical’ in summer but can correspond to ‘midlatitude’ air in winter
Sedimentation? Yes, but small
Swelling due to water vapor and temperature changes? Yes, but small outside the polar regions
Tropical SAGE seasonal cycle shows the importance of seasonality at the entry point; this propagates upward and poleward (see Niwano et al.)
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1970 1975 1980 1985 1990 1995 2000 2005
10-3
10-2
10-1
1970 1975 1980 1985 1990 1995 2000 2005
10-3
10-2
10-1
Hampton (37oN, 76oW) Garmisch (47oN, 11oE)
Stra
tosp
heri
c op
tical
dep
th, 5
32 n
m
Year
Latitude< 30o
> 30o
VolcanicEruptions
Lidar backscatter from 4 NDSC sites converted to extincion
Tropopause - 30 km
São José dos Campos(23oS, 46oW) Mauna Loa(20oN, 156oW))
17 - 30 km
Latitude< 30o
> 30o
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South polar aerosols: linked to synoptic conditions in troposphere, relationship to tropospheric cloud
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