Abstract. Strongly enhanced tropospheric ozone (O3) mixing ratios have
been reported in the Arabian Basin, a region with intense solar radiation
and high concentrations of O3 precursors such as nitrogen oxides (NOx) and
volatile organic compounds (VOCs). To analyze photochemical O3 production in the
marine boundary layer (MBL) around the Arabian Peninsula, we use shipborne
observations of NO, NO2, O3, OH, HO2, HCHO, the actinic flux,
water vapor, pressure and temperature obtained during the summer 2017 Air
Quality and Climate in the Arabian Basin (AQABA) campaign, and we compare them to
simulation results from the ECHAM-MESSy Atmospheric Chemistry (EMAC) general
circulation model. Net O3 production rates (NOPRs) were greatest over both the Gulf of Oman and the northern Red Sea (16 ppbv d−1) and
over the Arabian Gulf (32 ppbv d−1). The NOPR over the
Mediterranean, the southern Red Sea and the Arabian Sea did not
significantly deviate from zero; however, the results for the Arabian Sea
indicated weak net O3 production of 5 ppbv d−1 as well as net O3
destruction over the Mediterranean and the southern Red Sea with values of −1 and −4 ppbv d−1, respectively. Constrained
by HCHO∕NO2 ratios, our photochemistry calculations show that net O3
production in the MBL around the Arabian Peninsula mostly occurs in
NOx-limited regimes with a significant share of O3 production
occurring in the transition regime between NOx limitation and VOC limitation over
the Mediterranean and more significantly over the northern Red Sea and Oman
Gulf.