Increased aerosols can reverse Twomey effect in water clouds through radiative pathway

Abstract Aerosols play important roles in modulations of cloud properties and hydrological cycle by decreasing the size of cloud droplets with the increase of aerosols under the condition of fixed liquid water path, which is known as the first aerosol indirect effect or Twomey-effect or microphysica...

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Main Authors: Pradeep Khatri, Tadahiro Hayasaka, Brent N. Holben, Ramesh P. Singh, Husi Letu, Sachchida N. Tripathi
Format: Article
Language:English
Published: Nature Portfolio 2022-11-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-022-25241-y
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author Pradeep Khatri
Tadahiro Hayasaka
Brent N. Holben
Ramesh P. Singh
Husi Letu
Sachchida N. Tripathi
author_facet Pradeep Khatri
Tadahiro Hayasaka
Brent N. Holben
Ramesh P. Singh
Husi Letu
Sachchida N. Tripathi
author_sort Pradeep Khatri
collection DOAJ
description Abstract Aerosols play important roles in modulations of cloud properties and hydrological cycle by decreasing the size of cloud droplets with the increase of aerosols under the condition of fixed liquid water path, which is known as the first aerosol indirect effect or Twomey-effect or microphysical effect. Using high-quality aerosol data from surface observations and statistically decoupling the influence of meteorological factors, we show that highly loaded aerosols can counter this microphysical effect through the radiative effect to result both the decrease and increase of cloud droplet size depending on liquid water path in water clouds. The radiative effect due to increased aerosols reduces the moisture content, but increases the atmospheric stability at higher altitudes, generating conditions favorable for cloud top entrainment and cloud droplet coalescence. Such radiatively driven cloud droplet coalescence process is relatively stronger in thicker clouds to counter relatively weaker microphysical effect, resulting the increase of cloud droplet size with the increase of aerosol loading; and vice-versa in thinner clouds. Overall, the study suggests the prevalence of both negative and positive relationships between cloud droplet size and aerosol loading in highly polluted regions.
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spelling doaj.art-c739613f8a924f7295f9889a9bdfc9952022-12-22T02:48:46ZengNature PortfolioScientific Reports2045-23222022-11-0112111110.1038/s41598-022-25241-yIncreased aerosols can reverse Twomey effect in water clouds through radiative pathwayPradeep Khatri0Tadahiro Hayasaka1Brent N. Holben2Ramesh P. Singh3Husi Letu4Sachchida N. Tripathi5Center for Atmospheric and Oceanic Studies, Tohoku UniversityCenter for Atmospheric and Oceanic Studies, Tohoku UniversityNational Aeronautics and Space Administration, Goddard Space Flight CenterSchool of Life and Environmental Sciences, Schmid College of Science and Technology, Chapman UniversityInstitute of Remote Sensing and Digital Earth, Chinese Academy of SciencesDepartment of Civil Engineering, Indian Institute of Technology KanpurAbstract Aerosols play important roles in modulations of cloud properties and hydrological cycle by decreasing the size of cloud droplets with the increase of aerosols under the condition of fixed liquid water path, which is known as the first aerosol indirect effect or Twomey-effect or microphysical effect. Using high-quality aerosol data from surface observations and statistically decoupling the influence of meteorological factors, we show that highly loaded aerosols can counter this microphysical effect through the radiative effect to result both the decrease and increase of cloud droplet size depending on liquid water path in water clouds. The radiative effect due to increased aerosols reduces the moisture content, but increases the atmospheric stability at higher altitudes, generating conditions favorable for cloud top entrainment and cloud droplet coalescence. Such radiatively driven cloud droplet coalescence process is relatively stronger in thicker clouds to counter relatively weaker microphysical effect, resulting the increase of cloud droplet size with the increase of aerosol loading; and vice-versa in thinner clouds. Overall, the study suggests the prevalence of both negative and positive relationships between cloud droplet size and aerosol loading in highly polluted regions.https://doi.org/10.1038/s41598-022-25241-y
spellingShingle Pradeep Khatri
Tadahiro Hayasaka
Brent N. Holben
Ramesh P. Singh
Husi Letu
Sachchida N. Tripathi
Increased aerosols can reverse Twomey effect in water clouds through radiative pathway
Scientific Reports
title Increased aerosols can reverse Twomey effect in water clouds through radiative pathway
title_full Increased aerosols can reverse Twomey effect in water clouds through radiative pathway
title_fullStr Increased aerosols can reverse Twomey effect in water clouds through radiative pathway
title_full_unstemmed Increased aerosols can reverse Twomey effect in water clouds through radiative pathway
title_short Increased aerosols can reverse Twomey effect in water clouds through radiative pathway
title_sort increased aerosols can reverse twomey effect in water clouds through radiative pathway
url https://doi.org/10.1038/s41598-022-25241-y
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