Improving model representation of rapid ozone deposition over soil in the central Tibetan Plateau-Reference-Cited by-同舟云学术

Improving model representation of rapid ozone deposition over soil in the central Tibetan Plateau

Published:2024 Issue:2 Volume:4 Page:252-264
ISSN:2634-3606
Container-title:Environmental Science: Atmospheres
language:en
Short-container-title:Environ. Sci.: Atmos.

Author:

Zhang Chong¹^ORCID,Wang Jianshu¹,Zhang Yingjie¹^ORCID,Xu Wanyun²,Zhang Gen²,Miao Guofang³,Zhou Jiacheng⁴,Yu Hui⁴,Zhao Weixiong⁴^ORCID,Lin Weili⁵^ORCID,Kang Ling¹,Cai Xuhui¹,Zhang Hongsheng⁶,Ye Chunxiang¹^ORCID

Affiliation:

1. SKL-ESPC & SEPKL-AERM, College of Environmental Sciences and Engineering and Center for Environment and Science, Peking University, Beijing, China

2. State Key Laboratory of Severe Weather & Key Laboratory for Atmospheric Chemistry of CMA, Institute of Atmospheric Composition, Chinese Academy of Meteorological Sciences, Beijing, China

3. School of Geographical Sciences, Fujian Normal University, Fuzhou, China

4. Laboratory of Atmospheric Physico-Chemistry, Anhui Institute of Optics and Fine Mechanisms, Chinese Academy of Science, Hefei, Anhui, China

5. College of Life and Environmental Sciences, Minzu University of China, Beijing, China

6. Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, China

Abstract

Ozone deposition velocity with a daily mean of 0.49 cm s−1 was observed in the Tibetan Plateau and rationalized by local meteorological and soil conditions. Our research suggested widespread ozone deposition velocity over soil of 0.1–0.7 cm s−1.

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Publisher

Royal Society of Chemistry (RSC)

Link

http://pubs.rsc.org/en/content/articlepdf/2024/EA/D3EA00153A

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