The impact of the Himalayan aerosol factory: results from high resolution numerical modelling of pure biogenic nucleation over the Himalayan valleys

Observational data collected in December 2014 at the base camp of Mount Everest, Nepal, indicated frequent new particle formation events of pure biogenic origin. Those events were speculated to be controlled by the along-valley winds forming in the valley connecting the Indo-Gangetic plain to the observational site, the Nepal Climate Observatory-Pyramid. The valley winds funnel highly oxygenated organic molecules of biogenic origin to higher elevations where they nucleate. The mechanism was referred to as "The Himalayan aerosol factory". Its geographical extent and climate implications are currently unknown. In view of this, we conducted numerical chemical model simulations to corroborate the presence of the mechanism, and to quantify its geographical extent. Our numerical simulations confirmed that biogenic emissions located in the valleys can be converted into ultra-low volatility organic compounds, transported to the observational site by the along-valley winds, and therein nucleate. The overall time scale of the process, from the release of biogenic emissions to the conversion to ultra-low volatile organic compounds to the arrival time at the observational site, was found to be around 4 hours, consistent with the predicted along-valley winds intensity and the geographical distribution of biogenic emissions. A first estimation of the maximum injection height of biogenic particles, and highly oxygenated organic molecules, indicated the presence of efficient nucleating gases and biogenic particles at an elevation as high as 5000-6000 m a.s.l. These results suggest that the Himalayan chain, under specific weather conditions, is a main contributor to the biogenic aerosol loads in the free troposphere. Considering these findings, field campaigns, especially at the entrance of the valley's floors, and research consortia supporting atmospheric research in Asian mountain regions, are highly encouraged.

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Publication Details

Journal
Faraday Discussions
Published
2025-01-01
DOI
https://doi.org/10.1039/d4fd00171k
Citations
2
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
2.60

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article

The impact of the Himalayan aerosol factory: results from high resolution numerical modelling of pure biogenic nucleation over the Himalayan valleys

Markku Kulmala, Jaana Bäck, Bruno Vitali, Tuomo Nieminen et al.
2 citations
Faraday Discussions
Atmospheric chemistry and aerosols
2.60
article

The impact of the Himalayan aerosol factory: results from high resolution numerical modelling of pure biogenic nucleation over the Himalayan valleys

Markku Kulmala, Jaana Bäck, Bruno Vitali, Tuomo Nieminen, Douglas R. Worsnop, Alessandro Bigi, Angela Marinoni, Arineh Cholakian, Paolo Tuccella, Victoria A. Sinclair, Johannes Mikkola, Giancarlo Ciarelli, Dino Zardi, Federico Bianchi, Imad El Haddad, Bertrand Bessagnet, Hamish Gordon, Manuel Bettineschi
article en
2 citations

Abstract

Observational data collected in December 2014 at the base camp of Mount Everest, Nepal, indicated frequent new particle formation events of pure biogenic origin. Those events were speculated to be controlled by the along-valley winds forming in the valley connecting the Indo-Gangetic plain to the observational site, the Nepal Climate Observatory-Pyramid. The valley winds funnel highly oxygenated organic molecules of biogenic origin to higher elevations where they nucleate. The mechanism was referred to as "The Himalayan aerosol factory". Its geographical extent and climate implications are currently unknown. In view of this, we conducted numerical chemical model simulations to corroborate the presence of the mechanism, and to quantify its geographical extent. Our numerical simulations confirmed that biogenic emissions located in the valleys can be converted into ultra-low volatility organic compounds, transported to the observational site by the along-valley winds, and therein nucleate. The overall time scale of the process, from the release of biogenic emissions to the conversion to ultra-low volatile organic compounds to the arrival time at the observational site, was found to be around 4 hours, consistent with the predicted along-valley winds intensity and the geographical distribution of biogenic emissions. A first estimation of the maximum injection height of biogenic particles, and highly oxygenated organic molecules, indicated the presence of efficient nucleating gases and biogenic particles at an elevation as high as 5000-6000 m a.s.l. These results suggest that the Himalayan chain, under specific weather conditions, is a main contributor to the biogenic aerosol loads in the free troposphere. Considering these findings, field campaigns, especially at the entrance of the valley's floors, and research consortia supporting atmospheric research in Asian mountain regions, are highly encouraged.

Faraday DiscussionsVol. 258(0)
International Centre for Integrated Mountain Development (NP), University of Modena and Reggio Emilia (IT), Centre National de la Recherche Scientifique (FR), University of Helsinki (FI), École Polytechnique (FR), University of Trento (IT), University of L'Aquila (IT), Paul Scherrer Institute (CH), École Normale Supérieure - PSL (FR), Institute of Atmospheric Sciences and Climate (IT), Institut Pierre-Simon Laplace (FR), Ricerca sul Sistema Energetico (Italy) (IT), National Research Council (IT), Ferrari (Italy) (IT), Carnegie Mellon University (US)
Academy of Finland, HORIZON EUROPE Framework Programme, European Research Council, Jenny ja Antti Wihurin Rahasto
Openalex Percentile: Top 13%
Atmospheric chemistry and aerosols
2.60
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