Impact of stratospheric ozone on the subseasonal prediction in the southern hemisphere spring

Abstract Antarctic ozone has been regarded as a major driver of the Southern Hemisphere (SH) circulation change in the recent past. Here, we show that Antarctic ozone can also affect the subseasonal-to-seasonal (S2S) prediction during the SH spring. Its impact is quantified by conducting two reforec...

Full description

Bibliographic Details
Published in:Progress in Earth and Planetary Science
Main Authors: Jiyoung Oh, Seok-Woo Son, Jung Choi, Eun-Pa Lim, Chaim Garfinkel, Harry Hendon, Yoonjae Kim, Hyun-Suk Kang
Format: Article in Journal/Newspaper
Language:English
Published: SpringerOpen 2022
Subjects:
G
Online Access:https://doi.org/10.1186/s40645-022-00485-4
https://doaj.org/article/5645cf5566ed42c281036a21e4e0b2b1
Description
Summary:Abstract Antarctic ozone has been regarded as a major driver of the Southern Hemisphere (SH) circulation change in the recent past. Here, we show that Antarctic ozone can also affect the subseasonal-to-seasonal (S2S) prediction during the SH spring. Its impact is quantified by conducting two reforecast experiments with the Global Seasonal Forecasting System 5 (GloSea5). Both reforecasts are initialized on September 1st of each year from 2004 to 2020 but with different stratospheric ozone: one with climatological ozone and the other with year-to-year varying ozone. The reforecast with climatological ozone, which is common in the operational S2S prediction, shows the skill re-emergence in October after a couple of weeks of no prediction skill in the troposphere. This skill re-emergence, mostly due to the stratosphere–troposphere dynamical coupling, becomes stronger in the reforecast with year-to-year varying ozone. The surface prediction skill also increases over Australia. This result suggests that a more realistic stratospheric ozone could lead to improved S2S prediction in the SH spring.