Cause of a lower-tropospheric high-ozone layer in spring over Hanoi

Ogino, S., Miyazaki, K., Fujiwara, M., Nodzu, M., Shiotani, M., et al. (2022). Cause of a lower-tropospheric high-ozone layer in spring over Hanoi. Journal of Geophysical Research: Atmospheres, doi:https://doi.org/10.1029/2021JD035727

Title Cause of a lower-tropospheric high-ozone layer in spring over Hanoi
Genre Article
Author(s) S. Ogino, K. Miyazaki, M. Fujiwara, M. Nodzu, M. Shiotani, F. Hasebe, J. Matsumoto, Jacquelyn Witte, A. Thompson, H. Nguyen-Thi, T. Nguyen
Abstract The ozonesonde observations in Hanoi, Vietnam, over 14 years since 2004, have confirmed an enhancement in lower tropospheric ozone concentration at about 3 km altitude in the spring season. We investigated the evolution of the ozone enhancement from analysis of meteorological data, backward trajectories, and model sensitivity experiments. In spring, air masses over Hanoi exhibit strong height dependence. At 3 km, the high-ozone air masses originate from the land area to the west of Hanoi, while low-ozone air masses below about 1.5 km are from the oceanic area to the east. Above 4 km, the air masses are mostly traced back to the farther west area. The chemical transport model simulations revealed that precursor emissions from biomass burning in the inland Indochina Peninsula have the largest contribution to the lower tropospheric ozone enhancement, which is transported upward and eastward and overhangs the clean air intrusion from the ocean to the east of Hanoi. At this height level, the polluted air has the horizontal extent of about 20 degrees in longitude and latitude. The polluted air observed in Hanoi is transported further east and widely spread over the northern Pacific Ocean.
Publication Title Journal of Geophysical Research: Atmospheres
Publication Date May 27, 2022
Publisher's Version of Record https://doi.org/10.1029/2021JD035727
OpenSky Citable URL https://n2t.org/ark:/85065/d78p6481
OpenSky Listing View on OpenSky
EOL Affiliations ISF, SND

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