11A.4 Satellite (OMI) and Surface Observations Confirm Steady Decline of US NOx Emissions over the 2004-2017 Period

Thursday, 10 January 2019: 11:15 AM
North 124A (Phoenix Convention Center - West and North Buildings)
Rachel F. Silvern, Harvard Univ., Cambridge, MA; and D. J. Jacob, M. Sulprizio, L. J. Mickley, K. R. Travis, E. A. Marais, R. C. Cohen, J. L. Laughner, S. Choi, and J. Joiner

The National Emission Inventory (NEI) of the US EPA reports a steady decrease of US NOx emissions over the 2004-2017 period at a rate of -0.8 Mt a-1, reflecting sustained efforts to improve air quality. Tropospheric NO2 columns observed by the OMI satellite instrument over the US show a steady decrease until 2009 but a flattening afterward. This has been attributed to a decreasing effectiveness of NOx emission controls after 2009, implying that NEI trends are incorrect. We show here that the steady 2004-2017 decrease of NOx emissions reported by the NEI is in fact consistent with observed trends in nitrate wet deposition fluxes and surface NO2 concentrations when only sites with continuous records are considered. The post-2009 flattening of the OMI NO2 trend can be explained by an underestimate of background free tropospheric NO2 in the air mass factors (AMFs) used to account for increased satellite measurement sensitivity with altitude. This underestimate of background free tropospheric NO2 is supported by GEOS-Chem model simulations, SEAC4RS aircraft observations, and cloud-slicing OMI retrievals isolating free tropospheric NO2. As US NOx emissions decrease, background free tropospheric NO2 makes an increasing (and now dominant) relative contribution to the tropospheric columns measured from space. Steady decline of US NOx emissions over 2004-2017 is also consistent with the steady improvement of surface ozone air quality observed during that period. Better understanding is needed of the factors controlling free tropospheric NO2 in order to relate satellite observations of tropospheric NO2 columns to the underlying NOx emissions.
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