A11I-0183
Measurement and Modeling of Site-specific Nitrogen and Oxygen Isotopic Composition of Atmospheric Nitrous Oxide at Mace Head, Ireland
Monday, 14 December 2015
Poster Hall (Moscone South)
Michael J McClellan1, Eri Saikawa2, Ronald G Prinn3 and Shuhei Ono3, (1)Massachusetts Institute of Technology, Cambridge, MA, United States, (2)Emory University, Atlanta, GA, United States, (3)MIT, Cambridge, MA, United States
Abstract:
Global mixing ratios of atmospheric nitrous oxide (N
2O), a potent greenhouse gas, have increased nearly linearly from the beginning of the modern industrial period to today, with the current global average in excess of 325 ppb. This increase can be largely attributed to anthropogenic activity above the level of N
2O emissions from natural biotic sources. The effect of N
2O on Earth’s climate is twofold: in the troposphere, N
2O is radiatively active and chemically inert, while it serves as a reactive source of ozone-destroying nitrogen oxides in the stratosphere. The marked altitudinal divide in its reactivity means that all stages in the N
2O life cycle—emission, transport, and destruction—must be examined to understand the overall effect of N
2O on Earth’s climate. However, the understanding of the total impact of N
2O is incomplete, as there remain significant uncertainties in the global budget of this gas. Due to unique isotopic substitutions (
15N and
18O) made by different N
2O sources and stratospheric chemical reactions, the measurement of N
2O isotopic ratios in ambient air can help identify the distribution and magnitude of distinct source types. We present the first year of site-specific nitrogen and oxygen isotopic composition data from the MIT Stheno-tunable infrared direct absorption spectroscopy (TILDAS) instrument at Mace Head, Ireland. Aided by the Stheno preconcentration system, Stheno-TILDAS can achieve measurement precisions of 0.10‰ or greater for all isotopic ratios (δ
15N and δ
18O) in ambient N
2O. We further compare these data to the results from Model for Ozone and Related Tracers version 4 (MOZART-4) simulations, including N
2O isotopic fractionation processes and MERRA/GEOS-5 reanalysis meteorological fields. These results will form the basis of future Bayesian inverse modeling simulations that will constrain global N
2O source, circulation, and sink dynamics better.