Details

Autor(en) / Beteiligte

• Kim, Jeong-Hun
• Kim, Seong-Joong
• Youn, Daeok
• Kim, Maeng-Ki
• Kim, Joo-Hong
• Kim, Joowan
• Noh, El

Titel

Impact of North Atlantic-East Asian teleconnections on extremely high January PM10 cases in Korea

Ist Teil von

• Environmental pollution (1987), 2021-12, Vol.290, p.118051-118051, Article 118051

Ort / Verlag

Elsevier Ltd

Erscheinungsjahr

2021

Quelle

Alma/SFX Local Collection

Beschreibungen/Notizen

• In this study, we investigated the daily variability of PM10 concentrations in January in Korea during the past 19 years (2001–2019), as well as the associated atmospheric circulation patterns. The daily PM10 concentrations were classified into three cases: low (L; < 50 μg/m3), high (H; 50–100 μg/m3), and extremely high (EH; ≥ 100 μg/m3). We found that the strength of the East Asian winter monsoon influenced the PM10 variability in the L and H cases. However, the EH cases were strongly influenced by the rapid growth of barotropic warming (anticyclonic anomaly) over the eastern North Atlantic and Northern Europe (ENE), and the stationary Rossby waves grew rapidly over Eurasia within only four days. Analysis of the quasi-geostrophic geopotential tendency budget revealed that the anticyclonic anomaly over the ENE was enhanced by vorticity advection. Linear baroclinic model experiments confirmed that vorticity forcing over the ENE induces favorable atmospheric conditions for the occurrence of EH PM10 events in East Asia. As a result, the PM10 concentration sharply increased sharply by approximately three times over four days. This study suggests that understanding atmospheric teleconnections between the ENE and East Asia can effectively predict the occurrence of EH PM10 events in Korea, helping to reduce the human health risks from atmospheric pollution. [Display omitted] •Extremely high PM10 (EH) cases are associated with atmospheric stagnant pattern.•In EH cases, the PM10 concentration increased about 3 time in 4 days.•Stagnant patterns with EH cases are affected by the North Atlantic forcing.•North Atlantic anticyclonic anomaly forcing is developed by a vorticity advection.•The EH cases are induced by stagnant pattern through the Rossby wave propagation.