A Simple New Method for Calculating Precipitation Scavenging Effect on Particulate Matter: Based on Five-Year Data in Eastern China
A “rain-only” method is proposed to find out the precipitation effect on particle aerosol removal from the atmosphere, and this method is not only unique and novel but also very simple and can be easily adapted to predict aerosol particle scavenging over any region across the world irrespective of t...
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doaj-94362ee593b24a6395ec56bf2578d0472021-06-30T23:54:52ZengMDPI AGAtmosphere2073-44332021-06-011275975910.3390/atmos12060759A Simple New Method for Calculating Precipitation Scavenging Effect on Particulate Matter: Based on Five-Year Data in Eastern ChinaBin Zhou0Duanyang Liu1Wenlian Yan2Key Laboratory of Transportation Meteorology, China Meteorological Administration, Nanjing 210008, ChinaKey Laboratory of Transportation Meteorology, China Meteorological Administration, Nanjing 210008, ChinaKey Laboratory of Transportation Meteorology, China Meteorological Administration, Nanjing 210008, ChinaA “rain-only” method is proposed to find out the precipitation effect on particle aerosol removal from the atmosphere, and this method is not only unique and novel but also very simple and can be easily adapted to predict aerosol particle scavenging over any region across the world irrespective of the topographical, orographical, and climatic features. By using this simple method, the influences of the rain intensity and particle mass concentration on the aerosol scavenging efficiency are discussed. The results show that a higher concentration, a higher rain intensity, and a larger particle size lead to a higher scavenging efficiency and a higher scavenging rate. The greater the rain intensity, the higher the scavenging efficiency. The scavenging efficiency of PM<sub>10</sub> by precipitation is better than that of PM<sub>2.5</sub>. When the rain intensity is 10 mm h<sup>−1</sup>, the scavenging efficiency of PM<sub>2.5</sub> reaches 5.1 μg m<sup>−3</sup> h<sup>−1</sup>, and the scavenging efficiency of PM<sub>10</sub> reaches 15.8 μg m<sup>−3</sup> h<sup>−1</sup>. The scavenging rate increases faster when accumulative precipitation is below 15 mm. The scavenging rate has obvious monthly variation, and the scavenging rate of coastal areas is less than that of inland Jiangsu. The growth of the particle mass concentration after precipitation is divided into two stages: the rapid growth stage after precipitation ends, and the slow growth stage about 24 h after precipitation ends.https://www.mdpi.com/2073-4433/12/6/759air pollutionChinaparticulate matterprecipitation scavengingscavenging efficiencyscavenging rate |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Bin Zhou Duanyang Liu Wenlian Yan |
spellingShingle |
Bin Zhou Duanyang Liu Wenlian Yan A Simple New Method for Calculating Precipitation Scavenging Effect on Particulate Matter: Based on Five-Year Data in Eastern China Atmosphere air pollution China particulate matter precipitation scavenging scavenging efficiency scavenging rate |
author_facet |
Bin Zhou Duanyang Liu Wenlian Yan |
author_sort |
Bin Zhou |
title |
A Simple New Method for Calculating Precipitation Scavenging Effect on Particulate Matter: Based on Five-Year Data in Eastern China |
title_short |
A Simple New Method for Calculating Precipitation Scavenging Effect on Particulate Matter: Based on Five-Year Data in Eastern China |
title_full |
A Simple New Method for Calculating Precipitation Scavenging Effect on Particulate Matter: Based on Five-Year Data in Eastern China |
title_fullStr |
A Simple New Method for Calculating Precipitation Scavenging Effect on Particulate Matter: Based on Five-Year Data in Eastern China |
title_full_unstemmed |
A Simple New Method for Calculating Precipitation Scavenging Effect on Particulate Matter: Based on Five-Year Data in Eastern China |
title_sort |
simple new method for calculating precipitation scavenging effect on particulate matter: based on five-year data in eastern china |
publisher |
MDPI AG |
series |
Atmosphere |
issn |
2073-4433 |
publishDate |
2021-06-01 |
description |
A “rain-only” method is proposed to find out the precipitation effect on particle aerosol removal from the atmosphere, and this method is not only unique and novel but also very simple and can be easily adapted to predict aerosol particle scavenging over any region across the world irrespective of the topographical, orographical, and climatic features. By using this simple method, the influences of the rain intensity and particle mass concentration on the aerosol scavenging efficiency are discussed. The results show that a higher concentration, a higher rain intensity, and a larger particle size lead to a higher scavenging efficiency and a higher scavenging rate. The greater the rain intensity, the higher the scavenging efficiency. The scavenging efficiency of PM<sub>10</sub> by precipitation is better than that of PM<sub>2.5</sub>. When the rain intensity is 10 mm h<sup>−1</sup>, the scavenging efficiency of PM<sub>2.5</sub> reaches 5.1 μg m<sup>−3</sup> h<sup>−1</sup>, and the scavenging efficiency of PM<sub>10</sub> reaches 15.8 μg m<sup>−3</sup> h<sup>−1</sup>. The scavenging rate increases faster when accumulative precipitation is below 15 mm. The scavenging rate has obvious monthly variation, and the scavenging rate of coastal areas is less than that of inland Jiangsu. The growth of the particle mass concentration after precipitation is divided into two stages: the rapid growth stage after precipitation ends, and the slow growth stage about 24 h after precipitation ends. |
topic |
air pollution China particulate matter precipitation scavenging scavenging efficiency scavenging rate |
url |
https://www.mdpi.com/2073-4433/12/6/759 |
work_keys_str_mv |
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