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

• Main Authors: Y. Gonzalez, R. Commane, E. Manninen, B. C. Daube, L. D. Schiferl, J. B. McManus, K. McKain, E. J. Hintsa, J. W. Elkins, S. A. Montzka, C. Sweeney, F. Moore, J. L. Jimenez, P. Campuzano Jost, T. B. Ryerson, I. Bourgeois, J. Peischl, C. R. Thompson, E. Ray, P. O. Wennberg, J. Crounse, M. Kim, H. M. Allen, P. A. Newman, B. B. Stephens, E. C. Apel, R. S. Hornbrook, B. A. Nault, E. Morgan, S. C. Wofsy
• Format: Article
• Language: English
• Published: Copernicus Publications 2021-07-01
• Series: Atmospheric Chemistry and Physics
• Online Access: https://acp.copernicus.org/articles/21/11113/2021/acp-21-11113-2021.pdf
• ISSN: 1680-7316; 1680-7324

<p>We measured the global distribution of tropospheric N<span class="inline-formula">₂</span>O mixing ratios during the NASA airborne Atmospheric Tomography (ATom) mission. ATom measured concentrations of <span class="inline-formula">∼</span> 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<span class="inline-formula">₂</span>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<span class="inline-formula">₂</span>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<span class="inline-formula">₂</span>O mixing ratios in the troposphere is driven by the influence of N<span class="inline-formula">₂</span>O-depleted stratospheric air, especially at mid- and high latitudes. We observe the downward propagation of lower N<span class="inline-formula">₂</span>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<span class="inline-formula">₂</span>O mixing ratios occur close to the Equator, extending through the boundary layer and<span id="page11114"/> free troposphere. We observed influences from a complex and diverse mixture of N<span class="inline-formula">₂</span>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<span class="inline-formula">₂</span>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<span class="inline-formula">₂</span>O mixing ratios are mostly associated with pollution-related tracers arriving from the coastal area of Nigeria. Peaks of N<span class="inline-formula">₂</span>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<span class="inline-formula">₂</span>O global budget. The extensive data set from ATom will help improve the understanding of N<span class="inline-formula">₂</span>O emission processes and their representation in global models.</p>