Publications by authors named "Casper Labuschagne"

Article Synopsis
  • The Global Mercury Observation System (GMOS) started as a five-year initiative to monitor atmospheric mercury and evolved into a major program supporting global mercury observation efforts under the Minamata Convention.
  • The network consists of 28 ground-based monitoring stations that provide comprehensive data on mercury levels across various latitudes, from the Arctic to the Antarctic.
  • Analysis of mercury data from 2011 to 2020 revealed a significant north-south gradient in mercury concentrations, with notable seasonal variations and decreasing trends in certain remote areas.
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Environmental mercury (Hg) contamination is a global concern requiring action at national scales. Scientific understanding and regulatory policies are underpinned by global extrapolation of Northern Hemisphere Hg data, despite historical, political, and socioeconomic differences between the hemispheres that impact Hg sources and sinks. In this paper, we explore the primary anthropogenic perturbations to Hg emission and mobilization processes that differ between hemispheres and synthesize current understanding of the implications for Hg cycling.

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Unregulated chlorocarbons, here defined as dichloromethane (CHCl), perchloroethene (CCl), chloroform (CHCl), and methyl chloride (CHCl), are gases not regulated by the Montreal Protocol. While CHCl is the largest contributor of atmospheric chlorine, recent studies have shown that growth in emissions of the less abundant chlorocarbons could pose a significant threat to the recovery of the ozone layer. Despite this, there remain many regions for which no atmospheric monitoring exists, leaving gaps in our understanding of global emissions.

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Article Synopsis
  • Researchers at Cape Point, South Africa, measured atmospheric levels of HCFC-22, HFC-125, and HFC-152a for the first time in 2017, establishing baseline growth rates for these compounds.
  • The study identified Cape Town as the main source of emissions in southwestern South Africa, and used data along with population statistics to estimate national emissions for 2017.
  • Although South Africa's contribution to global emissions of these halocarbons is relatively low (under 2.5%), ongoing monitoring is necessary to ensure compliance with the Montreal Protocol regulations.
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The interplay between microbes and atmospheric physical and chemical conditions is an open field of research that can only be fully addressed using multidisciplinary approaches. The lack of coordinated efforts to gather data at representative temporal and spatial scales limits aerobiology to help understand large scale patterns of global microbial biodiversity and its causal relationships with the environmental context. This paper presents the sampling strategy and analytical protocols developed in order to integrate different fields of research such as microbiology, -omics biology, atmospheric chemistry, physics and meteorology to characterize atmospheric microbial life.

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Long-term monitoring of data of ambient mercury (Hg) on a global scale to assess its emission, transport, atmospheric chemistry, and deposition processes is vital to understanding the impact of Hg pollution on the environment. The Global Mercury Observation System (GMOS) project was funded by the European Commission (http://www.gmos.

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Wherever measurements have been made bromoform was found to be ubiquitous in the surface ocean in pmolar-nmolar concentrations. These measurements show concentrations in coastal regions orders of magnitude higher than in the pelagic oceans. Its atmospheric presence is primarily due to its release from algae and rapid transport to the marine boundary troposphere where it is known to participate in ozone chemistry via photochemical and catalytic pathways.

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Based on observed atmospheric carbon dioxide (CO2) concentration and an inverse method, we estimate that the Southern Ocean sink of CO2 has weakened between 1981 and 2004 by 0.08 petagrams of carbon per year per decade relative to the trend expected from the large increase in atmospheric CO2. We attribute this weakening to the observed increase in Southern Ocean winds resulting from human activities, which is projected to continue in the future.

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