On the dynamics of ozone depletion events at Villum Research Station in the High Arctic

Ozone depletion events (ODEs) occur every spring in the Arctic and have implications for the region's atmospheric oxidizing capacity, radiative balance, and mercury oxidation. Here, we comprehensively analyze ozone, ODEs, and their connection to meteorological and air mass history variables thr...

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Published in:Atmospheric chemistry and physics 2024-12, Vol.24 (23), p.13603-13631
Main Authors: Pernov, Jakob Boyd, Hjorth, Jens Liengaard, Sørensen, Lise Lotte, Skov, Henrik
Format: Article
Language:English
Subjects:
Accreditation
Aerosols
Air masses
Air pollution
Air temperature
Analysis
Arctic ozone
Arctic research
Depletion
Humidity
Ice
Machine learning
Mercury
Mixed layer
Oxidation
Ozone
Ozone depletion
Ozone layer depletion
Radiation
Ratios
Research centers
Sea ice
Sea ice temperatures
Statistical analysis
Statistical methods
Stratosphere
VOCs
Volatile organic compounds
Wind
Wind direction
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container_title Atmospheric chemistry and physics
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creator Pernov, Jakob Boyd
Hjorth, Jens Liengaard
Sørensen, Lise Lotte
Skov, Henrik
description Ozone depletion events (ODEs) occur every spring in the Arctic and have implications for the region's atmospheric oxidizing capacity, radiative balance, and mercury oxidation. Here, we comprehensively analyze ozone, ODEs, and their connection to meteorological and air mass history variables through statistical analyses, back trajectories, and machine learning (ML) at Villum Research Station, Station Nord, Greenland, from 1996 to 2019.
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subjects Accreditation
Aerosols
Air masses
Air pollution
Air temperature
Analysis
Arctic ozone
Arctic research
Depletion
Humidity
Ice
Machine learning
Mercury
Mixed layer
Oxidation
Ozone
Ozone depletion
Ozone layer depletion
Radiation
Ratios
Research centers
Sea ice
Sea ice temperatures
Statistical analysis
Statistical methods
Stratosphere
VOCs
Volatile organic compounds
Wind
Wind direction
title On the dynamics of ozone depletion events at Villum Research Station in the High Arctic
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