The Identification and Analysis of Long-Range Aerosol Transport Pathways with Layered Cloud-Aerosol Lidar with Orthogonal Polarization Datasets from 2006 to 2016

Author:

Wang Lingyu123,Wang Wensheng12ORCID,Lyu Baolei456,Zhang Jinghua12,Han Yilun3ORCID,Bai Yuqi3ORCID,Guo Zhi12

Affiliation:

1. Key Laboratory of Network Information System Technology (NIST), Institute of Electronics, Chinese Academy of Sciences, Beijing 100190, China

2. The Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100094, China

3. Department of Earth System Science, Ministry of Education Key Laboratory for Earth System Modeling, Institute for Global Change Studies, Tsinghua University, Beijing 100084, China

4. Huayun Sounding Meteorology Technology Corporation, Beijing 100081, China

5. Jiangsu Collaborative Innovation Center of Atmospheric Environment and Equipment Technology (CICAEET), Nanjing University of Information Science & Technology, Nanjing 210044, China

6. China Meteorological Administration Xiong’an Atmospheric Boundary Layer Key Laboratory, Xiong’an 071000, China

Abstract

In this study, we used Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) aerosol products acquired from 2006 to 2016 to identify global long-range aerosol transport pathways, including the trans-Atlantic, the trans-Pacific, and the trans-Arabian Sea pathways. Deep analyses were subsequently conducted focusing on two significant paths within the range of the trans-Pacific transport pathway, from which we generated a three-stage conceptual model mainly identifying aerosols from the Taklimakan Desert and aerosols from the North China Plain. The results show that in the first stage of the model, the dust or polluted-dust aerosols were emitted, raised, and mixed within the planetary boundary layer (PBL), characterized by high percentages (>70%) of aerosols in the PBL (AODPBL), while in the second stage, some aerosols were further raised into the free troposphere where the AODPBL percentages decreased to less than 40%, driven by vertical movements and turbulences; in the last stage, the aerosols gradually settled back to the surface layer due to gravity and wet deposition, inferred by increasing AODPBL percentages. We demonstrated that the proposed model is capable of characterizing different aerosol types and climate conditions on spatiotemporal scales, providing a straightforward and evident approach to exploring long-range aerosol transport pathways.

Funder

the China Postdoctoral Science Foundation

the Youth Innovation Promotion Association of Chinese Academy of Sciences

the Science and Technology Key Project of China Huayun Group

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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