On the Fate of Aerosols Produced by New Particle Formation in the Upper Troposphere and Lower Stratosphere

Abstract New particle formation (NPF) in the upper troposphere and lower stratosphere (UTLS) has been suggested to contribute to cloud condensation nuclei in the troposphere, as well as for maintaining the stratospheric aerosol layer over the Asian summer monsoon (ASM). However, the fate of newly formed particles and their potential impact on climate are largely unknown. Here we use in situ aircraft measurements of aerosol size distributions collected in the UTLS over the eastern ASM region, combined with Lagrangian trajectory modeling and satellite‐derived convection, to show that NPF events primarily occur downstream of convection in the upper troposphere (below the tropopause) between 350 and 360 K potential temperature levels. While the majority of air parcels containing NPF events descend into the lower troposphere, approximately 20% of NPF event parcels ascend into the stratosphere and thereby may contribute as a source of material to the stratospheric aerosol layer.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-07-24
DOI
https://doi.org/10.1029/2025gl116860
Citations
3
Primary Topic
Atmospheric Ozone and Climate
Type
article
Field-Weighted Citation Impact
3.90

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article

On the Fate of Aerosols Produced by New Particle Formation in the Upper Troposphere and Lower Stratosphere

T. P. Bui, Jonathan M. Dean‐Day, Matthew D. Brown, Luke D. Ziemba et al.
3 citations
Geophysical Research Letters
Atmospheric Ozone and Climate
3.90
article

On the Fate of Aerosols Produced by New Particle Formation in the Upper Troposphere and Lower Stratosphere

T. P. Bui, Jonathan M. Dean‐Day, Matthew D. Brown, Luke D. Ziemba, E. J. Jensen, Warren P. Smith, Rei Ueyama, Christina J. Williamson
article en
3 citations

Abstract

Abstract New particle formation (NPF) in the upper troposphere and lower stratosphere (UTLS) has been suggested to contribute to cloud condensation nuclei in the troposphere, as well as for maintaining the stratospheric aerosol layer over the Asian summer monsoon (ASM). However, the fate of newly formed particles and their potential impact on climate are largely unknown. Here we use in situ aircraft measurements of aerosol size distributions collected in the UTLS over the eastern ASM region, combined with Lagrangian trajectory modeling and satellite‐derived convection, to show that NPF events primarily occur downstream of convection in the upper troposphere (below the tropopause) between 350 and 360 K potential temperature levels. While the majority of air parcels containing NPF events descend into the lower troposphere, approximately 20% of NPF event parcels ascend into the stratosphere and thereby may contribute as a source of material to the stratospheric aerosol layer.

Geophysical Research LettersVol. 52(14)
NSF National Center for Atmospheric Research (US), Ames Research Center (US), Finnish Meteorological Institute (FI), Langley Research Center (US), University of Helsinki (FI), Cooperative Institute for Research in Environmental Sciences (US), University of Colorado Boulder (US), Bay Area Environmental Research Institute (US), NOAA Chemical Sciences Laboratory (US), Science and Technology Corporation (United States) (US)
National Science Foundation, National Aeronautics and Space Administration, Academy of Finland, Earth Sciences Division
Openalex Percentile: Top 6%
Atmospheric Ozone and Climate
3.90
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