Dominant Role of Arctic Dust With High Ice Nucleating Ability in the Arctic Lower Troposphere

Abstract Recent observations show that dust emitted within the Arctic (Arctic dust) has a remarkably high ice nucleating ability, especially between −20°C and −5°C, but its impacts on the number concentrations of ice nucleating particles (INPs) and radiative balance in the Arctic are not well unders...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Kei Kawai, Hitoshi Matsui, Yutaka Tobo
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
aerosol
Arctic dust
ice nucleating particles
mixed‐phase clouds
aerosol‐cloud interactions
radiative effect
Geophysics. Cosmic physics
QC801-809
Arctic
Online Access:https://doi.org/10.1029/2022GL102470
https://doaj.org/article/0a9e24b5d89b42e387dde5ef7c8c466e
Description
Summary:Abstract Recent observations show that dust emitted within the Arctic (Arctic dust) has a remarkably high ice nucleating ability, especially between −20°C and −5°C, but its impacts on the number concentrations of ice nucleating particles (INPs) and radiative balance in the Arctic are not well understood. Here we incorporate an observation‐based ice‐nucleation parameterization indicating the high ice nucleating ability of Arctic dust into a global aerosol‐climate model. A simulation using this parameterization better reproduces INP observations in the Arctic and estimates >100 times higher dust INP number concentrations with ∼100% contribution from Arctic dust in the Arctic lower troposphere (>60°N and >700 hPa) during summer and fall (June–November) than a simulation applying a standard ice‐nucleation parameterization suitable for desert dust to Arctic dust. Our results demonstrate the importance of considering an ice‐nucleation parameterization suitable for Arctic dust when simulating INPs and their effects on aerosol‐cloud interactions in the Arctic.

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