Quantifying nitrous oxide emissions from agriculture in the Midwest of
the U.S.
Abstract
Atmospheric nitrous oxide (N2O) is, after carbon dioxide and methane,
the third most important long-lived anthropogenic greenhouse gas in
terms of radiative forcing. Since preindustrial times a rising trend in
the global N2O concentrations is observed. Anthropogenic emissions of
N2O, mainly from agricultural activity, contribute considerably to this
trend. Sparse observational constraints have made it difficult to
quantify these emissions. The few studies on top-down approaches in the
U.S. that exist are mainly based on Lagrangian models and ground-based
measurements. They all propose a significant underestimation of
anthropogenic N2O emission sources in established inventories, such as
the Emissions Database for Global Atmospheric Research (EDGAR). In this
study we quantify anthropogenic N2O emissions in the Midwest of the
U.S., an area of high agricultural activity. In the course of the
Atmospheric Carbon and Transport – America (ACT-America) campaign
spanning from summer 2016 to summer 2019, an extensive dataset over four
seasons has been collected including in-situ N2O aircraft based
measurements in the lower and middle troposphere onboard NASA’s C-130
and B-200 aircraft. During fall 2017 and summer 2019 we conducted
measurements onboard the NASA-C130 with a
Quantum-Cascade-Laser-Spectrometer (QCLS) and on both aircraft over the
whole campaign flask measurements (NOAA) were collected. More than 300
joint flight hours were conducted and more than 500 flask samples were
collected over the U.S. Midwest. The QCLS system collected continuous
N2O data for approximately 60 flight hours in this region. The Eulerian
Weather Research and Forecasting model with chemistry enabled (WRF-Chem)
is being used to quantify regional agricultural N2O emissions using the
spatial characteristics of these atmospheric N2O mole fraction
observations. The numerical simulations enable potential surface
emission distributions to be compared to our airborne measurements, and
source estimates can be adjusted to minimize the differences, thus
quantifying N2O sources. These results are then compared to emission
rates in the EDGAR inventory.