4.7 Article

Investigating sources of ozone over California using AJAX airborne measurements and models.: Assessing the contribution from longrange transport

Journal

ATMOSPHERIC ENVIRONMENT
Volume 155, Issue -, Pages 53-67

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2017.02.008

Keywords

Ozone; Measurements and models; Stratospheric intrusion; Long-range transport from Asia; Surface impact

Funding

  1. NASA Postdoctoral Program
  2. Bay Area Environmental Research Institute
  3. Ames Research Center Director's funds
  4. NASA High-End Computing (HEC) Program through the NASA Advanced Super computing (NAS) Division at NASA Ames Research Center

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High ozone (03) concentrations at low altitudes (1.5-4 km) were detected from airborne Alpha Jet Atmospheric eXperiment (AJAX) measurements on 30 May 2012 off the coast of California (CA). We investigate the causes of those elevated 03 concentrations using airborne measurements and various models. GEOS-Chem simulation shows that the contribution from local sources is likely small. A back trajectory model was used to determine the air mass origins and how much they contributed to the 03 over CA. Low-level potential vorticity (PV) from Modern Era Retrospective analysis for Research and Applications 2 (MERRA-2) reanalysis data appears to be a result of the diabatic heating and mixing of airs in the lower altitudes, rather than be a result of direct transport from stratospheric intrusion. The Q diagnostic, which is a measure of the mixing of the air masses, indicates that there is sufficient mixing along the trajectory to indicate that 03 from the different origins is mixed and transported to the western U.S. The back-trajectory model simulation demonstrates the air masses of interest came mostly from the mid troposphere (MT, 76%), but the contribution of the lower troposphere (LT, 19%) is also significant compared to those from the upper troposphere/lower stratosphere (UT/LS, 5%). Air coming from the LT appears to be mostly originating over Asia. The possible surface impact of the high 03 transported aloft on the surface 03 concentration through vertical and horizontal transport within a few days is substantiated by the influence maps determined from the Weather Research and Forecasting Stochastic Time Inverted Lagrangian Transport (WRF-STILT) model and the observed increases in surface ozone mixing ratios. Contrasting this complex case with a stratospheric-dominant event emphasizes the contribution of each source to the high 03 concentration in the lower altitudes over CA. Integrated analyses using models, reanalysis, and diagnostic tools, allows high ozone values detected by in-situ measurements to be attributed to multiple source processes. (C) 2017 Elsevier Ltd. All rights reserved.

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