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Updated: Nov 20, 2025

An Ultra-clean Multilayer Apparatus for Collecting Size Fractionated Marine Plankton and Suspended Particles
Published on: April 19, 2018
New particle formation in the remote marine boundary layer
Guangjie Zheng1,2, Yang Wang1,3, Robert Wood4
1Center for Aerosol Science and Engineering, Department of Energy, Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, MO, USA.
New particle formation in marine boundary layers is more common than previously thought, especially after cold fronts. These new particles significantly influence cloud condensation nuclei and marine low clouds.
Area of Science:
- Atmospheric Science
- Climate Science
- Aerosol Science
Background:
- Marine low clouds are critical climate regulators.
- Cloud condensation nuclei (CCN) concentrations influence cloud properties.
- New particle formation (NPF) is a key global source of CCN.
Purpose of the Study:
- To investigate the occurrence and drivers of NPF in remote marine boundary layers.
- To understand the impact of NPF on CCN concentrations and marine low clouds.
Main Methods:
- Analysis of atmospheric conditions following cold front passages in remote marine environments.
- Observation of particle size distributions and growth.
- Assessment of meteorological and chemical factors influencing NPF.
Main Results:
- NPF occurs regularly and frequently in the upper marine boundary layer after cold fronts.
- Conditions favoring NPF include precipitation scavenging, low temperatures, gas transport, and high actinic flux.
- Newly formed particles grow and contribute significantly to CCN.
Conclusions:
- Cold front passages create favorable conditions for NPF in remote marine boundary layers.
- NPF in these regions is a substantial source of CCN, impacting marine low cloud properties and climate.
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