Synonyms: 
Atmospheric Tomography Mission
Associated content: 
ATom
Sub-categories: 
ATOM 2, ATom 3, ATOM 4, ATom Data Sets, ATom I

New SOA Treatments Within the Energy Exascale Earth System Model (E3SM): Strong Production and Sinks Govern Atmospheric SOA Distributions and Radiative Forcing

Lou, S., et al. (2020), New SOA Treatments Within the Energy Exascale Earth System Model (E3SM): Strong Production and Sinks Govern Atmospheric SOA Distributions and Radiative Forcing, J. Adv. Modeling Earth Syst., 12, e2020MS002266, doi:10.1029/2020MS002266.

Validation of satellite formaldehyde (HCHO) retrievals using observations from 12 aircraft campaigns

Zhu, L., et al. (2020), Validation of satellite formaldehyde (HCHO) retrievals using observations from 12 aircraft campaigns, Atmos. Chem. Phys., 20, 12329-12345, doi:10.5194/acp-20-12329-2020.

The potential role of organics in new particle formation and initial growth in the remote tropical upper troposphere

Straus, A., et al. (2020), The potential role of organics in new particle formation and initial growth in the remote tropical upper troposphere, Atmos. Chem. Phys., 20, 15037-15060, doi:10.5194/acp-20-15037-2020.

Interferences with aerosol acidity quantification due to gas-phase ammonia uptake onto acidic sulfate filter samples

Nault, B., et al. (2020), Interferences with aerosol acidity quantification due to gas-phase ammonia uptake onto acidic sulfate filter samples, Atmos. Meas. Tech., 13, 6193-6213, doi:10.5194/amt-13-6193-2020.

Laser Induced Fluorescence – Sulfur Dioxide

The LIF-SO2 instrument detects sulfur dioxide at the single-part per trillion (ppt) level using red-shifted laser-induced fluorescence. It has operated on the WB-57 and Global Hawk aircraft in the UT/LS, as well as on the DC-8. Sulfur Dioxide is an important precursor for aerosols including nucleation of new particles globally and can be greatly enhanced in the stratosphere following explosive volcanic eruptions. An important implication of the Asian Monsoon is transport of aerosol precursors including SO2 into the lower stratosphere.

Instrument Type: 
Fluorescence
Measurements: 
SO2
Aircraft: 
DC-8 - AFRC, WB-57 - JSC, Global Hawk - AFRC
Point(s) of Contact: 
Andrew Rollins (PI)

1.5 years of TROPOMI CO measurements: comparisons to MOPITT and ATom

Martínez-Alonso, S., et al. (2020), 1.5 years of TROPOMI CO measurements: comparisons to MOPITT and ATom, Atmos. Meas. Tech., 13, 4841-4864, doi:10.5194/amt-13-4841-2020.

Global Atmospheric Budget of Acetone: Air‐Sea Exchange and the Contribution to Hydroxyl Radicals

Wang, S., et al. (2020), Global Atmospheric Budget of Acetone: Air‐Sea Exchange and the Contribution to Hydroxyl Radicals, J. Geophys. Res., 125, e2020JD032553, doi:10.1029/2020JD032553.

Global-scale distribution of ozone in the remote troposphere from ATom and HIPPO airborne field missions.

Bourgeois, I., et al. (2020), Global-scale distribution of ozone in the remote troposphere from ATom and HIPPO airborne field missions., Atmos. Chem. Phys., doi:10.5194/acp-2020-315.

Airborne measurements of oxygen concentration from the surface to the lower stratosphere and pole to pole

Stephens, B., et al. (2021), Airborne measurements of oxygen concentration from the surface to the lower stratosphere and pole to pole, Atmos. Meas. Tech., 14, 2543-2574, doi:10.5194/amt-14-2543-2021.

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