Optical and Physical Characteristics of Aerosol Vertical Layers over Northeastern China

The optical and physical characteristics of the aerosol vertical layers over Northeastern China (NEC) are investigated using the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Level 2 layer products from 2007 to 2014. To better examine the spatial and temporal variations...

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Main Authors: Bo Su, Hao Li, Miao Zhang, Muhammad Bilal, Minxia Wang, Luqman Atique, Ziyue Zhang, Chun Zhang, Ge Han, Zhongfeng Qiu, Md. Arfan Ali
Format: Article
Language:English
Published: MDPI AG 2020-05-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/11/5/501
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author Bo Su
Hao Li
Miao Zhang
Muhammad Bilal
Minxia Wang
Luqman Atique
Ziyue Zhang
Chun Zhang
Ge Han
Zhongfeng Qiu
Md. Arfan Ali
author_facet Bo Su
Hao Li
Miao Zhang
Muhammad Bilal
Minxia Wang
Luqman Atique
Ziyue Zhang
Chun Zhang
Ge Han
Zhongfeng Qiu
Md. Arfan Ali
author_sort Bo Su
collection DOAJ
description The optical and physical characteristics of the aerosol vertical layers over Northeastern China (NEC) are investigated using the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Level 2 layer products from 2007 to 2014. To better examine the spatial and temporal variations in the characteristics of aerosols over NEC, the region is divided into three parts (Heilongjiang province, Jilin province, and Liaoning province) to analyze the inter-annual and seasonal variations of nine selected aerosol parameters in each part during night and day times. The results reveal that the values of aerosol optical depth (AOD) increase year by year, over the whole NEC, being relatively high over the Liaoning (LN) province; this might be induced by higher levels of economic development and agricultural activity. The highest AOD values appear in summer, which is plausibly related to the temperate monsoon climate in NEC. Higher AOD values exist during the daytime than at night; this is intuitively the result of higher daytime anthropogenic activities. The base altitude of the lowest aerosol layer (BAL) and the top altitude of the highest aerosol layer (TAH) varied significantly due to the topography of NEC. The number of aerosol layers (N) is relatively large over LN, which might be caused by a relatively stronger atmospheric convection over this landscape. The thickness of the lowest aerosol layer (TLL) bore little relationship with the topography of NEC. The AOD proportion of the lowest aerosol layer (PAODL) is high (0.70 to 0.85 for the entire NEC), indicating that aerosols are mainly concentrated in the lowest layer of the atmosphere. The volume depolarization ratio of the lowest aerosol layer (VDRL) is large during spring and winter due to the presence of dust aerosols. The color ratio of the lowest aerosol layer (CRL) is large during the day due to relatively more human activities taking place than at night. Moreover, there is a significantly positive linear correlation between N and TAH, and a negative logarithm correlation between N and PAODL over NEC. The results of this study could provide researchers and the government departments with detailed and certain optical and physical information about aerosol layers over NEC, to help in the treatment of air pollution over NEC.
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spelling doaj.art-f7834f50ae2847149ecdd602db05b37a2023-11-20T00:19:01ZengMDPI AGAtmosphere2073-44332020-05-0111550110.3390/atmos11050501Optical and Physical Characteristics of Aerosol Vertical Layers over Northeastern ChinaBo Su0Hao Li1Miao Zhang2Muhammad Bilal3Minxia Wang4Luqman Atique5Ziyue Zhang6Chun Zhang7Ge Han8Zhongfeng Qiu9Md. Arfan Ali10School of Earth Sciences and Engineering, Hohai University, Focheng West Road No. 8, Nanjing 210098, ChinaSchool of Earth Sciences and Engineering, Hohai University, Focheng West Road No. 8, Nanjing 210098, ChinaSchool of Environmental Science and Tourism, Nanyang Normal University, Wolong Road No. 1638, Nanyang 473061, ChinaSchool of Marine Sciences, Nanjing University of Information Science & Technology, Nanjing 210044, ChinaSchool of Environmental Science and Tourism, Nanyang Normal University, Wolong Road No. 1638, Nanyang 473061, ChinaSchool of Earth Sciences, Zhejiang University, Hangzhou 310027, ChinaSchool of Environmental Science and Tourism, Nanyang Normal University, Wolong Road No. 1638, Nanyang 473061, ChinaSchool of Environmental Science and Tourism, Nanyang Normal University, Wolong Road No. 1638, Nanyang 473061, ChinaSchool of Remote Sensing and Information Engineering, Wuhan University, Luoyu Road No. 129, Wuhan 430079, ChinaSchool of Marine Sciences, Nanjing University of Information Science & Technology, Nanjing 210044, ChinaSchool of Marine Sciences, Nanjing University of Information Science & Technology, Nanjing 210044, ChinaThe optical and physical characteristics of the aerosol vertical layers over Northeastern China (NEC) are investigated using the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) Level 2 layer products from 2007 to 2014. To better examine the spatial and temporal variations in the characteristics of aerosols over NEC, the region is divided into three parts (Heilongjiang province, Jilin province, and Liaoning province) to analyze the inter-annual and seasonal variations of nine selected aerosol parameters in each part during night and day times. The results reveal that the values of aerosol optical depth (AOD) increase year by year, over the whole NEC, being relatively high over the Liaoning (LN) province; this might be induced by higher levels of economic development and agricultural activity. The highest AOD values appear in summer, which is plausibly related to the temperate monsoon climate in NEC. Higher AOD values exist during the daytime than at night; this is intuitively the result of higher daytime anthropogenic activities. The base altitude of the lowest aerosol layer (BAL) and the top altitude of the highest aerosol layer (TAH) varied significantly due to the topography of NEC. The number of aerosol layers (N) is relatively large over LN, which might be caused by a relatively stronger atmospheric convection over this landscape. The thickness of the lowest aerosol layer (TLL) bore little relationship with the topography of NEC. The AOD proportion of the lowest aerosol layer (PAODL) is high (0.70 to 0.85 for the entire NEC), indicating that aerosols are mainly concentrated in the lowest layer of the atmosphere. The volume depolarization ratio of the lowest aerosol layer (VDRL) is large during spring and winter due to the presence of dust aerosols. The color ratio of the lowest aerosol layer (CRL) is large during the day due to relatively more human activities taking place than at night. Moreover, there is a significantly positive linear correlation between N and TAH, and a negative logarithm correlation between N and PAODL over NEC. The results of this study could provide researchers and the government departments with detailed and certain optical and physical information about aerosol layers over NEC, to help in the treatment of air pollution over NEC.https://www.mdpi.com/2073-4433/11/5/501aerosol layersAODCALIPSOnortheastern China
spellingShingle Bo Su
Hao Li
Miao Zhang
Muhammad Bilal
Minxia Wang
Luqman Atique
Ziyue Zhang
Chun Zhang
Ge Han
Zhongfeng Qiu
Md. Arfan Ali
Optical and Physical Characteristics of Aerosol Vertical Layers over Northeastern China
Atmosphere
aerosol layers
AOD
CALIPSO
northeastern China
title Optical and Physical Characteristics of Aerosol Vertical Layers over Northeastern China
title_full Optical and Physical Characteristics of Aerosol Vertical Layers over Northeastern China
title_fullStr Optical and Physical Characteristics of Aerosol Vertical Layers over Northeastern China
title_full_unstemmed Optical and Physical Characteristics of Aerosol Vertical Layers over Northeastern China
title_short Optical and Physical Characteristics of Aerosol Vertical Layers over Northeastern China
title_sort optical and physical characteristics of aerosol vertical layers over northeastern china
topic aerosol layers
AOD
CALIPSO
northeastern China
url https://www.mdpi.com/2073-4433/11/5/501
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