日本地球惑星科学連合2018年大会

講演情報

[JJ] 口頭発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS07] 成層圏・対流圏過程とその気候への影響

2018年5月23日(水) 10:45 〜 12:15 A07 (東京ベイ幕張ホール)

コンビーナ:渡辺 真吾(国立研究開発法人海洋研究開発機構)、河谷 芳雄(国立研究開発法人海洋研究開発機構)、関谷 高志(国立研究開発法人 海洋研究開発機構、共同)、佐藤 薫(東京大学 大学院理学系研究科 地球惑星科学専攻)、座長:関谷 高志

11:30 〜 11:45

[AAS07-10] Stratosphere-troposphere exchange of ozone and carbon monoxide over the northern Pacific Ocean using two chemical reanalysis data sets

*席 浩森1藤原 正智1宮崎 和幸2 (1.北海道大学大学院 地球環境科学院、2.独立行政法人 海洋研究開発機構 地球環境変動領域)

キーワード:成層圏対流圏大気交換、オゾン、一酸化炭素

Stratosphere-troposphere exchange (STE) is one of the important factors that determine the distribution of constituents in the troposphere and stratosphere. Two-way airmass exchange between the lower stratosphere and the troposphere occurs in association with mid-latitude weather disturbances, with the net transport from the stratosphere to troposphere. In this study, we analyze the STE over the northern hemisphere Pacific Ocean in northern winter, focusing on transport of ozone and carbon monoxide (CO) using two chemical reanalysis data sets, the Tropospheric Chemical Reanalysis version 1 (TCR-1) and the Monitoring Atmospheric Composition and Ccarbon monoxidelimate (MACC). The TCR-1 is a 10-year chemical reanalysis data set for the period from 2005 to 2014, while the MACC is for 2003 to 2012. Both reanalyses assimilate major satellite chemistry data during the respect periods. We calculate the amount of CO transported from troposphere-to-stratosphere (TST) and ozone transported from stratosphere-to-troposphere (STT) on the 350-K isentropic surface, by using 4 PVU potential vorticity to evaluate irreversible transport across the tropopause. Results from the analysis of TCR-1 data indicate that, the amount of ozone transport per case has a maximum in November and a minimum in February. It is also found that the amount of STT per case in years 2005-2008 is significantly smaller than that in years 2009-2014, and has a maximum in 2010 winter (from November 2010 to March 2011). In the presentation, we will show the seasonal dependence and 10-year changes of the ozone and CO transport, as well as intercomparison of the two different data sets.