Aerosol characteristics at the three poles of the Earth as characterized by Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations

To better understand the aerosol properties over the Arctic, Antarctic and Tibetan Plateau (TP), the aerosol optical properties were investigated using 13 years of CALIPSO (Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations) L3 data, and the back trajectories for air masses were also...

Full description

Bibliographic Details
Published in:Atmospheric Chemistry and Physics
Main Authors: Yang, Yikun, Zhao, Chuanfeng, Wang, Quan, Cong, Zhiyuan, Yang, Xingchuan, Fan, Hao
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/acp-21-4849-2021
https://acp.copernicus.org/articles/21/4849/2021/
id ftcopernicus:oai:publications.copernicus.org:acp90849
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:acp90849 2023-05-15T13:31:40+02:00 Aerosol characteristics at the three poles of the Earth as characterized by Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations Yang, Yikun Zhao, Chuanfeng Wang, Quan Cong, Zhiyuan Yang, Xingchuan Fan, Hao 2021-03-29 application/pdf https://doi.org/10.5194/acp-21-4849-2021 https://acp.copernicus.org/articles/21/4849/2021/ eng eng doi:10.5194/acp-21-4849-2021 https://acp.copernicus.org/articles/21/4849/2021/ eISSN: 1680-7324 Text 2021 ftcopernicus https://doi.org/10.5194/acp-21-4849-2021 2021-04-05T16:22:16Z To better understand the aerosol properties over the Arctic, Antarctic and Tibetan Plateau (TP), the aerosol optical properties were investigated using 13 years of CALIPSO (Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations) L3 data, and the back trajectories for air masses were also simulated using the Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) model. The results show that the aerosol optical depth (AOD) has obvious spatial- and seasonal-variation characteristics, and the aerosol loading over Eurasia, Ross Sea and South Asia is relatively large. The annual-average AODs over the Arctic, Antarctic and TP are 0.046, 0.024 and 0.098, respectively. Seasonally, the AOD values are larger from late autumn to early spring in the Arctic, in winter and spring in the Antarctic, and in spring and summer over the TP. There are no significant temporal trends of AOD anomalies in the three study regions. Clean marine and dust-related aerosols are the dominant types over ocean and land, respectively, in both the Arctic and Antarctic, while dust-related aerosol types have greater occurrence frequency (OF) over the TP. The OF of dust-related and elevated smoke is large for a broad range of heights, indicating that they are likely transported aerosols, while other types of aerosols mainly occurred at heights below 2 km in the Antarctic and Arctic. The maximum OF of dust-related aerosols mainly occurs at 6 km altitude over the TP. The analysis of back trajectories of the air masses shows large differences among different regions and seasons. The Arctic region is more vulnerable to mid-latitude pollutants than the Antarctic region, especially in winter and spring, while the air masses in the TP are mainly from the Iranian Plateau, Tarim Basin and South Asia. Text Antarc* Antarctic Arctic Ross Sea Copernicus Publications: E-Journals Antarctic Arctic Ross Sea The Antarctic Atmospheric Chemistry and Physics 21 6 4849 4868
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description To better understand the aerosol properties over the Arctic, Antarctic and Tibetan Plateau (TP), the aerosol optical properties were investigated using 13 years of CALIPSO (Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations) L3 data, and the back trajectories for air masses were also simulated using the Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT) model. The results show that the aerosol optical depth (AOD) has obvious spatial- and seasonal-variation characteristics, and the aerosol loading over Eurasia, Ross Sea and South Asia is relatively large. The annual-average AODs over the Arctic, Antarctic and TP are 0.046, 0.024 and 0.098, respectively. Seasonally, the AOD values are larger from late autumn to early spring in the Arctic, in winter and spring in the Antarctic, and in spring and summer over the TP. There are no significant temporal trends of AOD anomalies in the three study regions. Clean marine and dust-related aerosols are the dominant types over ocean and land, respectively, in both the Arctic and Antarctic, while dust-related aerosol types have greater occurrence frequency (OF) over the TP. The OF of dust-related and elevated smoke is large for a broad range of heights, indicating that they are likely transported aerosols, while other types of aerosols mainly occurred at heights below 2 km in the Antarctic and Arctic. The maximum OF of dust-related aerosols mainly occurs at 6 km altitude over the TP. The analysis of back trajectories of the air masses shows large differences among different regions and seasons. The Arctic region is more vulnerable to mid-latitude pollutants than the Antarctic region, especially in winter and spring, while the air masses in the TP are mainly from the Iranian Plateau, Tarim Basin and South Asia.
format Text
author Yang, Yikun
Zhao, Chuanfeng
Wang, Quan
Cong, Zhiyuan
Yang, Xingchuan
Fan, Hao
spellingShingle Yang, Yikun
Zhao, Chuanfeng
Wang, Quan
Cong, Zhiyuan
Yang, Xingchuan
Fan, Hao
Aerosol characteristics at the three poles of the Earth as characterized by Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations
author_facet Yang, Yikun
Zhao, Chuanfeng
Wang, Quan
Cong, Zhiyuan
Yang, Xingchuan
Fan, Hao
author_sort Yang, Yikun
title Aerosol characteristics at the three poles of the Earth as characterized by Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations
title_short Aerosol characteristics at the three poles of the Earth as characterized by Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations
title_full Aerosol characteristics at the three poles of the Earth as characterized by Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations
title_fullStr Aerosol characteristics at the three poles of the Earth as characterized by Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations
title_full_unstemmed Aerosol characteristics at the three poles of the Earth as characterized by Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations
title_sort aerosol characteristics at the three poles of the earth as characterized by cloud–aerosol lidar and infrared pathfinder satellite observations
publishDate 2021
url https://doi.org/10.5194/acp-21-4849-2021
https://acp.copernicus.org/articles/21/4849/2021/
geographic Antarctic
Arctic
Ross Sea
The Antarctic
geographic_facet Antarctic
Arctic
Ross Sea
The Antarctic
genre Antarc*
Antarctic
Arctic
Ross Sea
genre_facet Antarc*
Antarctic
Arctic
Ross Sea
op_source eISSN: 1680-7324
op_relation doi:10.5194/acp-21-4849-2021
https://acp.copernicus.org/articles/21/4849/2021/
op_doi https://doi.org/10.5194/acp-21-4849-2021
container_title Atmospheric Chemistry and Physics
container_volume 21
container_issue 6
container_start_page 4849
op_container_end_page 4868
_version_ 1766020082430902272