Impact of stratospheric air and surface emissions on tropospheric nitrous oxide during ATom

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Gonzalez, Yenny, Commane, Róisín, Manninen, Ethan, Daube, Bruce C., Schiferl, Luke D., McManus, J. Barry, McKain, Kathryn, Hintsa, Eric J., Elkins, James W., Montzka, Stephen A., Sweeney, Colm, Moore, Fred, Jimenez, Jose L., Campuzano Jost, Pedro, Ryerson, Thomas B., Bourgeois, Ilann, Peischl, Jeff, Thompson, Chelsea R., Ray, Eric, Wennberg, Paul O., Crounse, John, Kim, Michelle, Allen, Hannah M., Newman, Paul A., Stephens, Britton B., Apel, Eric C., Hornbrook, Rebecca S., Nault, Benjamin A., Morgan, Eric, Wofsy, Steven C.
• Format: Text
• Language: English
• Published: 2021
• Subjects: Arctic; Pacific; Southern Ocean; Atlantic Arctic; Atlantic-Arctic
• Online Access: https://doi.org/10.5194/acp-21-11113-2021; https://acp.copernicus.org/articles/21/11113/2021/

We measured the global distribution of tropospheric N 2 O mixing ratios during the NASA airborne Atmospheric Tomography (ATom) mission. ATom measured concentrations of ∼ 300 gas species and aerosol properties in 647 vertical profiles spanning the Pacific, Atlantic, Arctic, and much of the Southern Ocean basins, nearly from pole to pole, over four seasons (2016–2018). We measured N 2 O concentrations at 1 Hz using a quantum cascade laser spectrometer (QCLS). We introduced a new spectral retrieval method to account for the pressure and temperature sensitivity of the instrument when deployed on aircraft. This retrieval strategy improved the precision of our ATom QCLS N 2 O measurements by a factor of three (based on the standard deviation of calibration measurements). Our measurements show that most of the variance of N 2 O mixing ratios in the troposphere is driven by the influence of N 2 O-depleted stratospheric air, especially at mid- and high latitudes. We observe the downward propagation of lower N 2 O mixing ratios (compared to surface stations) that tracks the influence of stratosphere–troposphere exchange through the tropospheric column down to the surface. The highest N 2 O mixing ratios occur close to the Equator, extending through the boundary layer and free troposphere. We observed influences from a complex and diverse mixture of N 2 O sources, with emission source types identified using the rich suite of chemical species measured on ATom and the geographical origin calculated using an atmospheric transport model. Although ATom flights were mostly over the oceans, the most prominent N 2 O enhancements were associated with anthropogenic emissions, including from industry (e.g., oil and gas), urban sources, and biomass burning, especially in the tropical Atlantic outflow from Africa. Enhanced N 2 O mixing ratios are mostly associated with pollution-related tracers arriving from the coastal area of Nigeria. Peaks of N 2 O are often associated with indicators of photochemical processing, suggesting possible unexpected source processes. In most cases, the results show how difficult it is to separate the mixture of different sources in the atmosphere, which may contribute to uncertainties in the N 2 O global budget. The extensive data set from ATom will help improve the understanding of N 2 O emission processes and their representation in global models.