selected presentation from the instaar monday noon seminar...
TRANSCRIPT
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Selected Presentation from the INSTAAR Monday Noon Seminar Series.
Institute of Arctic and Alpine Research, University of Colorado at Boulder.http://instaar.colorado.edu
http://instaar.colorado.edu/other/seminar_mon_presentations
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03 Feb. 2003 Detlev Helmig, INSTAAR and Program in Atmospheric and Oceanic Sciences (PAOS)Email: [email protected]"New insights into snow-photochemical processes and snow-atmosphere gas exchange (if you ever wonder whatmay happen in your freezer if the light stays on)."Seminar given at INSTAAR, University of Colorado. Copyright 2003 Detlev Helmig. All Rights Reserved.Helmig presentation (2.2 Mb PDF).
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Selected Presentation from the INSTAAR Monday Noon Seminar Series.
Institute of Arctic and Alpine Research, University of Colorado at Boulder.http://instaar.colorado.edu
http://instaar.colorado.edu/other/seminar_mon_presentations
03 Feb. 2003 Detlev Helmig, INSTAAR and Program in Atmospheric and Oceanic Sciences (PAOS) Email:[email protected]"New insights into snow-photochemical processes and snow-atmosphere gas exchange (if you ever wonder whatmay happen in your freezer if the light stays on)."Seminar given at INSTAAR, University of Colorado. Copyright 2003 Detlev Helmig. All Rights Reserved.Helmig presentation (2.2 Mb PDF).
Abstract
Snowpack has been considered a rather inert substrate that undergoes little chemical interaction with the atmosphere. The conservation of gases in interstitial air and ice cores has been used to decipher records of past atmosphericcomposition and climate. Over the past decade an increasing number of previously unknown snow-photochemicalreactions have been discovered. These processes have been shown to affect the surface-atmosphere exchange of manytrace gases and may have implications on the interpretation of ice core records.
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Inert ???
No next day hangover
Deficient in active properties; especially lacking a usual or
anticipated chemical or biological action
Having no or little activity to react
Having no effect
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Detlev Helmig
�
"New Insights into Snow-Photochemical Processes and Snow-Atmosphere Gas Exchange“
(if you ever wondered what may happen in your freezer in case the light stays on)
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Carina in the freezer
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Ice Core Measurements
CO2
Methane
Nitrous Oxide (N2O)
CO
Hydrogen Peroxide (H2O2)
Formaldehyde (H2CO)
Methyl Bromide (CH3Br)
Chlorofluorocarbons (CFC)
Methanesulfonate (MSA)
Oxygen
Nitrogen
Argon
Anions: Cl-, NO3-, SO4
2-,
Cations: Ca2+, K+, Mg2+, Na+, NH4+
Others: Fe, S, Al, Si, Ti, Mg
18O in H2O14C in CO14C in CO215N in N236Cl10Be
Primary Aerosol
Electrical Conductivity (balance of acids and bases)
Minerals (Silicates, Clay, Mirca, Feldspars, etc.)
Microparticles, Dust
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Pristine Arctic?
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Pollution in the Arctic
• Lead Records in Greenland Ice Cores
• Heavy Metals (Lead, Hg) in Fish, Mammals
• Pesticides (DDT, Lindan) in Birds, Mammals
• Environmental Pollutants (PCB, PCP) in Wildlife
• Antarctic (Arctic) Ozone Hole
• Hg in Arctic Environment
• Polar Sunrise Ozone Depletion
• ??? Nitrogen Photochemistry ???
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Front Cover AE
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Polar Springtime Ozone Depletion (Alert)
Bottenheim et al., Atmos Environ. 36, 2535 (2002)
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X Barrow
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Polar Ozone Depletion Chemistry
1. Formation of Br2
(HOBr)g -> (HOBr)aq
(HOBr)aq + H+
aq + Br-aq -> (Br2)aq + H2O
(Br2)aq -> (Br2)g
2. Ozone Destruction
Br2 + hn -> 2 Br
2 Br + 2 O3 -> 2 BrO + 2 O2
3. Recycling of BrO
a) BrO + BrO -> 2 Br + O2
b) OH + CO (or VOC) -> HO2 + CO2 (or VOC products)
BrO + HO2 -> HOBr + O2
HOBr + hn -> Br + OH
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BrO/Ozone
Honninger and Platt, Atmos. Environ. 36, 2481 (2002)
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Ozone Depletion in Arctic Snowpack
Diurnal Ozone and NOx at 30 cm depth
Peterson and Honrath, GRL 28, 511, 2001
Ozone in Firn Air
NOx in Firn Air
Solar Actinic Flux
NOx in Ambient Air
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Sun/Shading Experiments
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Actinic Flux into Snowpack
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Shepson et al., AGU, 2000
CH3CO-O-O-NO2
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CO production in snow
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Chemical Fluxes out of the Snow at Summit
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NO at South Pole
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Photochemical Cycles
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Photochemical Ozone Production
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Photochemical Ozone Production
Summit Diurnal Photochemical Ozone Production: 1.8 – 2.6 ppb/day
South Pole Diurnal Photochemical Ozone Production: 3 - 5 ppb/day (Crawford et al., GRL 28, 3641 (2001)
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OH at South Pole
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Photochemical Ozone Production
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Ambient Ozone at South Pole
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Ozone Depletion in Arctic Snowpack
Peterson and Honrath, GRL 28, 511, 2001
Ozone in Firn Air
NOx in Firn Air
Solar Actinic Flux
NOx in Ambient Air
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Ozone Fluxes out of Seasonal Snow
Zeller, 2000
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Table 1
Literature with ozone deposition measurements over snow-covered surfaces.
Reference Location Landscape Measurement Dep. Velo- Comments
Technique city (cm s-1)
Aldaz, 1969 New Mexico BE 0.02
Galbally & Allison, 1972
Mt Buller, Australia
1.3 m Snow Depth
TG -3.3 - 1.7 Ozone release from snow observed.
Galbally and Roy, 1980a,b
Australia TG, BE 0.06 Deposition velocity increased with snow age.
Wesely et al., 1981
Illinois Plowed Field ECM*, CL 0.03 (mean)
Colbeck & Harrison, 1985
Lancaster/England
Grass Field TG, CL 0.08
Padro et al. 1992 Canada Deciduous Forest
ECM 0.3
Stocker et al., 1995
Colorado Grassland ECM, CL 0.04-0.1 Deposition velocity decreased with snow age.
Zeller & Hehn, 1996
Wyoming Coniferous Forest
ECM, CL Consistent upwards ozone fluxes observed.
Gong et al., 1997 Camp Narwahl
Ice Camp TB 0.006 – 0.3 Data for ozone depletion events (Polar Sunrise)
Zeller, 2000 Wyoming Coniferous Forest
ECM, CL Upwards ozone fluxes from
surface (mean 0.2 mg m-2
s-1
)
*BE: Box Enclosure; ECM :Eddy Correl. Method; CL: Chemiluminescence; TG: Tower Gradient; TB: Teth. Balloon
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Ozone in the Arctic Boundary Layer at Summit, Greenland
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Instrumentation for Tethered Balloon Vertical Profiling
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Summit Surface Ozone Measurements
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Ozone Diurnal Trends at Summit
52.5
53.5
54.5
55.5
0:00 3:00 6:00 9:00 12:00 15:00 18:00 21:00 0:00
Time (hrs)
Diu
rnal M
ean
Ozo
ne (
pp
b)
5
6
7
8
0:00 3:00 6:00 9:00 12:00 15:00 18:00 21:00 0:00
Time (hrs)
Sta
nd
. D
ev
. o
f D
iura
l M
ea
ns
(p
pb
)
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Summit June 10, 2000 Profiling Data
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Summit Potential Temperature Profile June 10, 2000
0
100
200
300
400
500
600
700
288 289 290 291 292 293 294 295 296
Potential Temperature (K)
Heig
ht
(m)
Up, 16:14
Down, 16:38
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Boundary Layer
Height
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Summit Ozone/RH Profile June 18, 2000
Profile Mixing Temp Temp WS WS ozone Ozone Richardson Stability Ozone Ozone
Layer Height 2/3 MLH 1/3 MLH 2/3 MLH 1/3 MLH 2/3 MLH 1/3 MLH Number Function Flux Dep. Vel.
m K K m/s m/s ppb ppb kg/(s m2) cm/s
8up 70 259.70 259.90 7.30 6.00 50.80 50.40 -0.10 2.09 -5.58E-10 0.77
42up 75 258.50 258.70 4.20 4.10 53.20 51.00 -18.97 72.89 -8.19E-09 11.08
43up 74 259.43 259.66 3.90 3.80 56.80 56.30 -21.44 79.89 -2.04E-09 2.54
Flight #43up TS Potential
Temperature
0
10
20
30
40
50
60
70
80
90
100
290 291 292 293
Flight #43up TS Temperature
0
10
20
30
40
50
60
70
80
90
100
259 259.5 260
Flight #43up TS Wind Speed
0
10
20
30
40
50
60
70
80
90
100
1 2 3 4 5
Flight # 43up - ECC Ozone
0
10
20
30
40
50
60
70
80
90
100
54 56 58 60
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Surface Data/Balloon Sonde Comparison
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Summit 3D Potential Temperature
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Summit 3D Wind Speed
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Summary
NO HONO Cl, F CO Alkenes HCHO H2O2 PAN?
NO2 HNO2 H3CCHO
HNO3
Aerosols
NO3-, Organics
Ozone
???
Mechanisms? Seasonality? Magnitude of Fluxes? Seasonal Snow <-> Year-Round Snow?
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Summit 2000
Niwot Ridge
Summit
Coastal Greenland?
2003-2006Future Flux
Research
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South Pole
2003/2004
Future Balloon Research
ANTCI
Antarctic Tropospheric Chemistry Investigation
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Contributors
Jim Boulter
Florence Bocquet
Don David
Nancy Rivera Garymar Rivera
Doug Hultstrand
Scott Peckham
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