| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6340628 | Atmospheric Environment | 2013 | 9 Pages |
Abstract
Source from Taiwan contributes more than half of the high O3 concentration over northwestern Taiwan prior to frontal passage during the first episode, but decreases to mostly below 40% over western Taiwan during the second episode when Asian outflow occurs, and increases to more than 60% over central and southwestern Taiwan due to pollution accumulation under an anticyclonic departure.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Atmospheric Science
Authors
Fujung Tsai, Tsun-Hsien Liu,
