Abstract

The Cape Verde Atmospheric Observatory (CVAO), which is influenced by both, marine and desert dust air masses, has been used for long-term measurements of different properties of the atmospheric aerosol from 2008 to 2017. These properties include particle number size distributions (PNSD), light absorbing carbon (LAC) and concentrations of cloud condensation nuclei (CCN) together with their hygroscopicity. Here we summarize the results obtained for these properties and use an unsupervised machine learning algorithm for the classification of aerosol types. Five types of aerosols, i.e., marine, freshly-formed, mixture, moderate dust and heavy dust, were classified. Air masses during marine periods are from the Atlantic Ocean and during dust periods are from the Sahara. Heavy dust was more frequently present during wintertime, whereas the clean marine periods were more frequently present during springtime. It was observed that during the dust periods CCN number concentrations at a supersaturation of 0.30 % are roughly 2.5 times higher than during marine periods, but the hygroscopicity (κ) of particles in the size range from ∼30 to ∼175 nm during marine and dust periods are comparable. The long-term data presented here, together with the aerosol classification, can be used as a base to improve our understanding of annual cycles of the atmospheric aerosol in the eastern tropical Atlantic and on aerosol-cloud interactions and it can be used as a base for driving, evaluating and constraining atmospheric model simulations.

Highlights

  • We summarize the results obtained for these properties and use an unsu[5] pervised machine learning algorithm for the classification of aerosol types

  • Air masses during marine periods are from the Atlantic Ocean and during dust periods are from the Sahara

  • After classification based on machine learning, we found five different aerosol clusters for the 10 year-long data 15 set obtained at Cape Verde Atmospheric Observatory (CVAO) – marine, freshly-formed, mixture, moderate dust and heavy dust

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Summary

Introduction

15 Aerosol particles are known to impact the cloud formation, life cycle of clouds and global radiative forcing. These impacts are closely related to aerosol particle physical and chemical properties. Natural aerosol sources include primary mineral dust, sea spray, and wildfire aerosol, as well as precursors for new particle formation, such as sulfur- and carbon-containing gases from vegetation, ocean environment, and volcanoes, that can subsequently form 20 particles in the atmosphere (Carslaw et al, 2010). Mineral dust is likely the most abundant aerosol type by mass in the atmosphere (Kok et al, 2017), with estimates for the dust emission ranging from 1000-2150 Tg yr−1 (Zender et al, 2004).

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