A semi-Lagrangian view of ozone production tendency in North American outflow in the summers of 2009 and 2010

作者：Zhang B; Owen R C^*; Perlinger J A; Kumar A; Wu S; Martin M Val; Kramer L; Helmig D; Honrath R E

来源：Atmospheric Chemistry and Physics, 2014, 14(5): 2267-2287.

DOI：10.5194/acp-14-2267-2014

The Pico Mountain Observatory, located at 2225 m a.s.l. in the Azores Islands, was established in 2001 to observe long-range transport from North America to the central North Atlantic. In previous research conducted at the observatory, ozone enhancement (%26gt; 55 ppbv) in North American outflows was observed, and efficient ozone production in these outflows was postulated. This study is focused on determining the causes for high d[O-3] / d[CO] values (similar to 1 ppbv ppbv(-1)) observed in the summers of 2009 and 2010. The folded retroplume technique, developed by Owen and Honrath ( 2009), was applied to combine upwind FLEXPART transport pathways with GEOS-Chem chemical fields. The folded result provides a semi-Lagrangian view of polluted North American outflow in terms of physical properties and chemical processes, including production/loss rate of ozone and NOx produced by lightning and thermal decomposition of peroxy acetyl nitrate ( PAN). Two transport events from North America were identified for detailed analysis. High d[O-3] / d[CO] was observed in both events, but due to differing transport mechanisms, ozone production tendency differed between the two. A layer of net ozone production was found at 2 km a.s.l. over the Azores in the first event plume, apparently driven by PAN decomposition during subsidence of air mass in the Azores-Bermuda High. In the second event, net ozone loss occurred during transport in the lower free troposphere, yet observed d[O-3] / d[ CO] was high. We estimate that in both events, CO loss through oxidation contributed significantly to d[O-3] / d[CO] enhancement. Thus, it is not appropriate to use CO as a passive tracer of pollution in these events. In general, use of d[O-3] / d[CO] as an indicator of net ozone production/loss may be invalid for any situation in which oxidants are elevated. Based on our analysis, use of d[O-3] / d[CO] to diagnose ozone enhancement without verifying the assumption of negligible CO loss is not advisable.

• 出版日期2014