Influence of aerosols on lightning activities in central eastern parts of China

Abstract Time series data of lightning flash rates, aerosol optical depth (AOD), surface relative humidity, potential temperature, and convective available potential energy (CAPE) for 14 consecutive summers (2001–2014) over central eastern parts of China (32.5°–40°N, 100°–120°E) have been analyzed t...

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Main Authors: Zheng Shi, HaiChao Wang, YongBo Tan, LuYing Li, ChunSun Li
Format: Article
Language:English
Published: Wiley 2020-02-01
Series:Atmospheric Science Letters
Subjects:
Online Access:https://doi.org/10.1002/asl.957
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spelling doaj-e7449caeebd0479ea8ab55f487c06f872020-11-25T02:04:06ZengWileyAtmospheric Science Letters1530-261X2020-02-01212n/an/a10.1002/asl.957Influence of aerosols on lightning activities in central eastern parts of ChinaZheng Shi0HaiChao Wang1YongBo Tan2LuYing Li3ChunSun Li4Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC‐FEMD)/Key Laboratory for Aerosol‐Cloud‐Precipitation of China Meteorological Administration Nanjing University of Information Science & Technology Nanjing ChinaKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC‐FEMD)/Key Laboratory for Aerosol‐Cloud‐Precipitation of China Meteorological Administration Nanjing University of Information Science & Technology Nanjing ChinaKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC‐FEMD)/Key Laboratory for Aerosol‐Cloud‐Precipitation of China Meteorological Administration Nanjing University of Information Science & Technology Nanjing ChinaKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC‐FEMD)/Key Laboratory for Aerosol‐Cloud‐Precipitation of China Meteorological Administration Nanjing University of Information Science & Technology Nanjing ChinaKey Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC‐FEMD)/Key Laboratory for Aerosol‐Cloud‐Precipitation of China Meteorological Administration Nanjing University of Information Science & Technology Nanjing ChinaAbstract Time series data of lightning flash rates, aerosol optical depth (AOD), surface relative humidity, potential temperature, and convective available potential energy (CAPE) for 14 consecutive summers (2001–2014) over central eastern parts of China (32.5°–40°N, 100°–120°E) have been analyzed to investigate the impact of aerosol on the lightning flash rate. The Pearson correlation and the partial correlation are used to study the linear correlations between the lightning flash rate and AOD, potential temperature, surface relative humidity, and CAPE. The results show that the lightning flash rate is positively correlated (r = .64) with AOD under relatively clean conditions (AOD < 1.0), which may result from aerosol microphysical effect. In the situation of high aerosol concentration (AOD > 1.0), the correlation between AOD and lightning flash rate is not obvious (r = −.06), which may be due to the radiation effect of aerosol and the decrease of the number of large ice particles caused by excessive aerosol concentration. CAPE and surface relative humidity are both positively correlated with the lightning flash rates under relatively clean (AOD < 1.0) and relatively polluted (AOD > 1.0) conditions. Potential temperature is moderate positively correlated with the lightning flash rate under relatively clean conditions (r = .51, AOD < 1.0) but shows no significant linear relationship under relatively polluted conditions (r = .07, AOD > 1.0).https://doi.org/10.1002/asl.957aerosolcloud microphysicscorrelation coefficientlightning activity
collection DOAJ
language English
format Article
sources DOAJ
author Zheng Shi
HaiChao Wang
YongBo Tan
LuYing Li
ChunSun Li
spellingShingle Zheng Shi
HaiChao Wang
YongBo Tan
LuYing Li
ChunSun Li
Influence of aerosols on lightning activities in central eastern parts of China
Atmospheric Science Letters
aerosol
cloud microphysics
correlation coefficient
lightning activity
author_facet Zheng Shi
HaiChao Wang
YongBo Tan
LuYing Li
ChunSun Li
author_sort Zheng Shi
title Influence of aerosols on lightning activities in central eastern parts of China
title_short Influence of aerosols on lightning activities in central eastern parts of China
title_full Influence of aerosols on lightning activities in central eastern parts of China
title_fullStr Influence of aerosols on lightning activities in central eastern parts of China
title_full_unstemmed Influence of aerosols on lightning activities in central eastern parts of China
title_sort influence of aerosols on lightning activities in central eastern parts of china
publisher Wiley
series Atmospheric Science Letters
issn 1530-261X
publishDate 2020-02-01
description Abstract Time series data of lightning flash rates, aerosol optical depth (AOD), surface relative humidity, potential temperature, and convective available potential energy (CAPE) for 14 consecutive summers (2001–2014) over central eastern parts of China (32.5°–40°N, 100°–120°E) have been analyzed to investigate the impact of aerosol on the lightning flash rate. The Pearson correlation and the partial correlation are used to study the linear correlations between the lightning flash rate and AOD, potential temperature, surface relative humidity, and CAPE. The results show that the lightning flash rate is positively correlated (r = .64) with AOD under relatively clean conditions (AOD < 1.0), which may result from aerosol microphysical effect. In the situation of high aerosol concentration (AOD > 1.0), the correlation between AOD and lightning flash rate is not obvious (r = −.06), which may be due to the radiation effect of aerosol and the decrease of the number of large ice particles caused by excessive aerosol concentration. CAPE and surface relative humidity are both positively correlated with the lightning flash rates under relatively clean (AOD < 1.0) and relatively polluted (AOD > 1.0) conditions. Potential temperature is moderate positively correlated with the lightning flash rate under relatively clean conditions (r = .51, AOD < 1.0) but shows no significant linear relationship under relatively polluted conditions (r = .07, AOD > 1.0).
topic aerosol
cloud microphysics
correlation coefficient
lightning activity
url https://doi.org/10.1002/asl.957
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