4.7 Article

Tropical Cyclones Reduce Ozone in the Tropopause Region Over the Western Pacific: An Analysis of 18 Years Ozonesonde Profiles

Journal

EARTHS FUTURE
Volume 9, Issue 2, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020EF001635

Keywords

ozone; ozonesonde; tropical cyclones; tropopause layer; western Pacific

Funding

  1. National Key Research and Development Program of China [2018YFC1505703]
  2. Strategic Priority Research Program of Chinese Academy of Sciences [XDA17010102]
  3. National Natural Science Foundation of China [91837311, 41975050, 41675040]
  4. European Community [603557]
  5. international Postdoctoral Exchange Fellowship Program 2017 [20171015]

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This study quantitatively assesses the impact of western Pacific typhoons on ozone in the upper troposphere and lower stratosphere. Results show that typhoons negatively affect ozone concentrations in Hong Kong and Naha, with vertical transport by intense typhoons causing even larger negative anomalies. Horizontal transport within the Asian summer monsoon anticyclone also contributes to the low ozone values measured in the region.
Typhoons play a key role in causing low ozone concentrations in the upper troposphere and lower stratosphere (UTLS) over the western Pacific. In this study, 18 years records (2000-2017) of balloon-borne ozone measurements in Hong Kong (22.3 degrees N, 114.2 degrees E) and Naha (26.2 degrees N, 127.7 degrees E) are combined with trajectory calculations to quantitatively assess the impact of western Pacific typhoons on ozone in the UTLS. The results show that 46.3% (44.9%) of the ozone profiles in Hong Kong (Naha) are impacted by western Pacific typhoons from July to October, with negative ozone anomalies exceeding -20%. Vertical transport by intense typhoons affects 16.8% (18.8%) of the ozone profiles in Hong Kong (Naha) with even larger negative anomalies (<-40%). Vertical transport of tropical cyclones reduces ozone by about 20-60 ppbv compared to the mean ozone profile near the tropopause. Ozone values below 60 ppbv in the upper troposphere in Hong Kong and Naha are mainly caused by the uplift in the western Pacific typhoons and by horizontal transport within the Asian summer monsoon (ASM) anticyclone. The horizontal transport in the ASM anticyclone has larger contributions to the low ozone values measured over Hong Kong than over Naha.

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