Sulfur dioxide in the tropical marine boundary layer: dry deposition and heterogeneous oxidation observed during the Pacific Atmospheric Sulfur Experiment

Research flights with the National Center for Atmospheric Research (NCAR) C-130 airborne laboratory were conducted over the equatorial ocean during the Pacific Atmospheric Sulfur Experiment (PASE). The focused, repetitive flight plans provided a unique opportunity to explore the principal pathways o...

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Published inJournal of atmospheric chemistry Vol. 63; no. 1; pp. 13 - 32
Main Authors Faloona, Ian, Conley, Stephen A, Blomquist, Byron, Clarke, Antony D, Kapustin, Vladimir, Howell, Steven, Lenschow, Don H, Bandy, Alan R
Format Journal Article
LanguageEnglish
Published Dordrecht Dordrecht : Springer Netherlands 01.05.2009
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Springer Nature B.V
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Abstract Research flights with the National Center for Atmospheric Research (NCAR) C-130 airborne laboratory were conducted over the equatorial ocean during the Pacific Atmospheric Sulfur Experiment (PASE). The focused, repetitive flight plans provided a unique opportunity to explore the principal pathways of sulfur processing in remote marine environments in close detail. Fast airborne measurements of SO₂ using the Drexel University APIMS (Atmospheric Pressure Ionization Mass Spectrometer) instrument further provided unprecedented insight into the complete budget of this important sulfur gas. In general, turbulent mixing in the marine boundary layer (MBL) continuously depletes SO₂ due to the shallow convection of the tropical trade wind regime by venting the gas into the buffer layer (BuL) above. However, on nearly one-third of the flights a net import of SO₂ into the MBL from the BuL was observed. Concurrent measurements of the DMS budget allowed for a heterogeneous S(IV) oxidation rate to be inferred from the SO₂ budget residual. The average heterogeneous loss rate was found to be 0.05 h⁻¹, which taken in conjunction with the observed aerosol surface area distributions and O₃ levels indicates that the supermicron aerosols maintain a near neutral pH. The average dry deposition velocity of SO₂ was found to be 0.4 cm s⁻¹, about 30% lower than predicted by standard parameterizations. The yield of SO₂ from DMS oxidation was found to be near unity. The mission averages indicate that approximately 57% of the SO₂ in the MBL is lost to aerosols, 27% is subject to dry deposition, 7% is mixed into the BuL, and 10% is oxidized by OH.
AbstractList Research flights with the National Center for Atmospheric Research (NCAR) C-130 airborne laboratory were conducted over the equatorial ocean during the Pacific Atmospheric Sulfur Experiment (PASE). The focused, repetitive flight plans provided a unique opportunity to explore the principal pathways of sulfur processing in remote marine environments in close detail. Fast airborne measurements of SO 2 using the Drexel University APIMS (Atmospheric Pressure Ionization Mass Spectrometer) instrument further provided unprecedented insight into the complete budget of this important sulfur gas. In general, turbulent mixing in the marine boundary layer (MBL) continuously depletes SO 2 due to the shallow convection of the tropical trade wind regime by venting the gas into the buffer layer (BuL) above. However, on nearly one-third of the flights a net import of SO 2 into the MBL from the BuL was observed. Concurrent measurements of the DMS budget allowed for a heterogeneous S(IV) oxidation rate to be inferred from the SO 2 budget residual. The average heterogeneous loss rate was found to be 0.05 h −1 , which taken in conjunction with the observed aerosol surface area distributions and O 3 levels indicates that the supermicron aerosols maintain a near neutral pH. The average dry deposition velocity of SO 2 was found to be 0.4 cm s −1 , about 30% lower than predicted by standard parameterizations. The yield of SO 2 from DMS oxidation was found to be near unity. The mission averages indicate that approximately 57% of the SO 2 in the MBL is lost to aerosols, 27% is subject to dry deposition, 7% is mixed into the BuL, and 10% is oxidized by OH.
Research flights with the National Center for Atmospheric Research (NCAR) C-130 airborne laboratory were conducted over the equatorial ocean during the Pacific Atmospheric Sulfur Experiment (PASE). The focused, repetitive flight plans provided a unique opportunity to explore the principal pathways of sulfur processing in remote marine environments in close detail. Fast airborne measurements of SO sub(2) using the Drexel University APIMS (Atmospheric Pressure Ionization Mass Spectrometer) instrument further provided unprecedented insight into the complete budget of this important sulfur gas. In general, turbulent mixing in the marine boundary layer (MBL) continuously depletes SO sub(2) due to the shallow convection of the tropical trade wind regime by venting the gas into the buffer layer (BuL) above. However, on nearly one-third of the flights a net import of SO sub(2) into the MBL from the BuL was observed. Concurrent measurements of the DMS budget allowed for a heterogeneous S(IV) oxidation rate to be inferred from the SO sub(2) budget residual. The average heterogeneous loss rate was found to be 0.05h super(-1), which taken in conjunction with the observed aerosol surface area distributions and O sub(3) levels indicates that the supermicron aerosols maintain a near neutral pH. The average dry deposition velocity of SO sub(2) was found to be 0.4cms super(-1), about 30% lower than predicted by standard parameterizations. The yield of SO sub(2) from DMS oxidation was found to be near unity. The mission averages indicate that approximately 57% of the SO sub(2) in the MBL is lost to aerosols, 27% is subject to dry deposition, 7% is mixed into the BuL, and 10% is oxidized by OH.
Research flights with the National Center for Atmospheric Research (NCAR) C-130 airborne laboratory were conducted over the equatorial ocean during the Pacific Atmospheric Sulfur Experiment (PASE). The focused, repetitive flight plans provided a unique opportunity to explore the principal pathways of sulfur processing in remote marine environments in close detail. Fast airborne measurements of SO₂ using the Drexel University APIMS (Atmospheric Pressure Ionization Mass Spectrometer) instrument further provided unprecedented insight into the complete budget of this important sulfur gas. In general, turbulent mixing in the marine boundary layer (MBL) continuously depletes SO₂ due to the shallow convection of the tropical trade wind regime by venting the gas into the buffer layer (BuL) above. However, on nearly one-third of the flights a net import of SO₂ into the MBL from the BuL was observed. Concurrent measurements of the DMS budget allowed for a heterogeneous S(IV) oxidation rate to be inferred from the SO₂ budget residual. The average heterogeneous loss rate was found to be 0.05 h⁻¹, which taken in conjunction with the observed aerosol surface area distributions and O₃ levels indicates that the supermicron aerosols maintain a near neutral pH. The average dry deposition velocity of SO₂ was found to be 0.4 cm s⁻¹, about 30% lower than predicted by standard parameterizations. The yield of SO₂ from DMS oxidation was found to be near unity. The mission averages indicate that approximately 57% of the SO₂ in the MBL is lost to aerosols, 27% is subject to dry deposition, 7% is mixed into the BuL, and 10% is oxidized by OH.
Research flights with the National Center for Atmospheric Research (NCAR) C-130 airborne laboratory were conducted over the equatorial ocean during the Pacific Atmospheric Sulfur Experiment (PASE). The focused, repetitive flight plans provided a unique opportunity to explore the principal pathways of sulfur processing in remote marine environments in close detail. Fast airborne measurements of SO^sub 2^ using the Drexel University APIMS (Atmospheric Pressure Ionization Mass Spectrometer) instrument further provided unprecedented insight into the complete budget of this important sulfur gas. In general, turbulent mixing in the marine boundary layer (MBL) continuously depletes SO^sub 2^ due to the shallow convection of the tropical trade wind regime by venting the gas into the buffer layer (BuL) above. However, on nearly one-third of the flights a net import of SO^sub 2^ into the MBL from the BuL was observed. Concurrent measurements of the DMS budget allowed for a heterogeneous S(IV) oxidation rate to be inferred from the SO^sub 2^ budget residual. The average heterogeneous loss rate was found to be 0.05 h^sup -1^, which taken in conjunction with the observed aerosol surface area distributions and O^sub 3^ levels indicates that the supermicron aerosols maintain a near neutral pH. The average dry deposition velocity of SO^sub 2^ was found to be 0.4 cm s^sup -1^, about 30% lower than predicted by standard parameterizations. The yield of SO^sub 2^ from DMS oxidation was found to be near unity. The mission averages indicate that approximately 57% of the SO^sub 2^ in the MBL is lost to aerosols, 27% is subject to dry deposition, 7% is mixed into the BuL, and 10% is oxidized by OH.[PUBLICATION ABSTRACT]
Author Lenschow, Don H
Blomquist, Byron
Bandy, Alan R
Faloona, Ian
Kapustin, Vladimir
Clarke, Antony D
Conley, Stephen A
Howell, Steven
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Issue 1
Keywords Sulfur cycle
S(IV) oxidation
Dry deposition
Marine boundary layer
Sea salt aerosols
dimethyl sulfide
Atmospheric fallout
biogeochemical cycle
Marine atmosphere
aerosols
tropical zone
oxidation
Measurement campaign
Deposition rate
mass spectroscopy
Chemical reaction kinetics
Sulfur dioxide
Chemical ionization
Atmospheric chemistry
Atmospheric boundary layer
Aircraft observation
Shallow convection
Heterogeneous reaction
Language English
License CC BY 4.0
LinkModel DirectLink
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ObjectType-Feature-1
content type line 14
ObjectType-Article-1
ObjectType-Feature-2
content type line 23
OpenAccessLink https://doi.org/10.1007/s10874-010-9155-0
PQID 365745931
PQPubID 54153
PageCount 20
ParticipantIDs proquest_miscellaneous_745639596
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Springer Netherlands
Springer
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Snippet Research flights with the National Center for Atmospheric Research (NCAR) C-130 airborne laboratory were conducted over the equatorial ocean during the Pacific...
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SubjectTerms Aerosols
Airborne particulates
Atmospheric aerosols
Atmospheric boundary layer
Atmospheric chemistry
Atmospheric Protection/Air Quality Control/Air Pollution
Atmospheric research
Atmospheric Sciences
Boundary layers
Chemical composition and interactions. Ionic interactions and processes
Convection, turbulence, diffusion. Boundary layer structure and dynamics
Dry deposition
Earth and Environmental Science
Earth Sciences
Earth, ocean, space
Exact sciences and technology
External geophysics
Ionization
Marine boundary layer
Marine environment
Meteorology
Oxidation
S(IV) oxidation
Sea salt aerosols
Sulfur
Sulfur cycle
Sulfur dioxide
Trade winds
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Title Sulfur dioxide in the tropical marine boundary layer: dry deposition and heterogeneous oxidation observed during the Pacific Atmospheric Sulfur Experiment
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