Abstract. Chemical mechanisms describe how emissions of gases and particles evolve in
the atmosphere and are used within chemical transport models to evaluate
past, current, and future air quality. Thus, a chemical mechanism must
provide robust and accurate predictions of air pollutants if it is to be
considered for use by regulatory bodies. In this work, we provide an initial
evaluation of the Community Regional Atmospheric Chemistry Multiphase
Mechanism (CRACMMv1.0) by assessing CRACMMv1.0 predictions of surface ozone
(O3) across the northeastern US during the summer of 2018 within the
Community Multiscale Air Quality (CMAQ) modeling system. CRACMMv1.0 O3
predictions of hourly and maximum daily 8 h average (MDA8) ozone were
lower than those estimated by the Regional Atmospheric Chemistry Mechanism with aerosol module 6
(RACM2_ae6), which better matched surface network
observations in the northeastern US (RACM2_ae6 mean bias of
+4.2 ppb for all hours and +4.3 ppb for MDA8; CRACMMv1.0 mean bias of
+2.1 ppb for all hours and +2.7 ppb for MDA8). Box model calculations
combined with results from CMAQ emission reduction simulations indicated
a high sensitivity of O3 to compounds with biogenic sources. In addition,
these calculations indicated the differences between CRACMMv1.0 and
RACM2_ae6 O3 predictions were largely explained by
updates to the inorganic rate constants (reflecting the latest assessment
values) and by updates to the representation of monoterpene chemistry.
Updates to other reactive organic carbon systems between
RACM2_ae6 and CRACMMv1.0 also affected ozone predictions and
their sensitivity to emissions. Specifically, CRACMMv1.0 benzene, toluene,
and xylene chemistry led to efficient NOx cycling such that CRACMMv1.0 predicted controlling aromatics reduces ozone without rural O3
disbenefits. In contrast, semivolatile and intermediate-volatility alkanes
introduced in CRACMMv1.0 acted to suppress O3 formation across the
regional background through the sequestration of nitrogen oxides (NOx)
in organic nitrates. Overall, these analyses showed that the CRACMMv1.0 mechanism within the CMAQ model was able to reasonably simulate ozone
concentrations in the northeastern US during the summer of 2018 with similar
magnitude and diurnal variation as the current operational Carbon Bond
(CB6r3_ae7) mechanism and good model performance compared to recent
modeling studies in the literature.