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Decrease in Nucleated Particles and Cloud Condensation Nuclei Observed across a Range of Environments

delete2026-04-27
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OA
AI
D
Do-Hyeon Park
P
Paolo Laj
E
Elisabeth Andrews
C
Clémence Rose
A
Angela Benedetti
M
Markku Kulmala
I
Inés Zabala
E
Erik Ahlberg
A
Andrés Alástuey
E
Eija Asmi
O
Olaf Bath
T
Tak Wai Chan
J
Jin-soo Choi
M
Martine Collaud Coen
S
Sébastien Conil
S
Sebastiao Martins Dos Santos
K
Konstantinos Eleftheriadis
M
Markus Fiebig
M
Maria I. Gini
A
A. Gannet Hallar
A
Antti Hyvärinen
L
Leena Järvi
N
Nikos Kalivitis
M
Melita Keywood
J
Jeong Eun Kim
S
Sumin Kim
J
Jenni Kontkanen
G
Giorgos Kouvarakis
A
Adam Kristensson
C
Chongai Kuang
M
Meehye Lee
H
Heikki Lihavainen
Y
Yong Lin
C
Chris Lunder
A
Atsushi Matsuki
O
Olga L. Mayol-Bracero
M
Maik Merkel
N
Nikolaos Mihalopoulos
C
Cathrine Lund Myhre
J
Jin-soo Park
M
Minsu Park
R
Rokjin J. Park
T
Tuukka Petäja
J
Jean-Philippe Putaud
A
Andreas Schwerin
K
Karine Sellegri
E
Erik Swietlicki
T
Thomas Tuch
P
Peter Tunved
V
Ville Vakkari
P
Paolo Villani
S
Stergios Vratolis
K
Kay Weinhold
A
Alfred Wiedensohler
Y
Young Jun Yoon
S
Seong Soo Yum
V
Vladimir Zdimal
J
John A. Ogren
S
Sang‐Woo Kim *
DOI:10.1021/acs.est.5c18035delete
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Abstract

Abstract

En 中文
Understanding new particle formation (NPF) and the fate of nanoparticles is crucial because of their close links to air quality, cloud formation, and climate. These effects vary spatially and temporally owing to diverse aerosol sources and their relatively short atmospheric lifetime. Here, we present a comprehensive analysis of long-term trends in NPF-associated nucleation-mode particles and cloud condensation nuclei (CCN) concentrations across diverse observation environments using quality-controlled particle number size distribution (PNSD) and CCN data from 37 sites, primarily from Global Atmosphere Watch (GAW) stations. We identify declining decadal trends in both NPF occurrences and nucleated particle concentrations across most site types, with the strongest declines in urban areas. We observe simultaneous reductions in both CCN concentrations and nucleation-mode particles, suggesting that newly formed particles are a potential source of CCN. This, in turn, suggests that cloud microphysical properties and radiative effects can be indirectly influenced through aerosol–cloud interactions that modify cloud droplet formation. These findings indicate that decreasing anthropogenic emissions could influence the climate forcing potential of aerosol–cloud interactions, with important implications for future climate projections.
Keywords:
Aerosols
Climate
Condensation
Nanoparticles
Redox reactions
new particle formation
particle number size distribution
cloud condensation nuclei
aerosol−cloud interactions
air quality regulations

Journal

E
ENVIRONMENTAL SCIENCE & TECHNOLOGY
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11.3
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2.1K
Citations:
1

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Seoul National University
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Korea University
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finnish meteorological institute
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University of Utah
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stockholm university
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University of Helsinki
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Lund University
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Environment and Climate Change Canada
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