| Literature DB >> 30245704 |
Francesca Sprovieri1, Nicola Pirrone2, Mariantonia Bencardino1, Francesco D'Amore1, Francesco Carbone1, Sergio Cinnirella1, Valentino Mannarino1, Matthew Landis3, Ralf Ebinghaus4, Andreas Weigelt4, Ernst-Günther Brunke5, Casper Labuschagne5, Lynwill Martin5, John Munthe6, Ingvar Wängberg6, Paulo Artaxo7, Fernando Morais7, Henrique de Melo Jorge Barbosa7, Joel Brito7, Warren Cairns8, Carlo Barbante8,9, María Del Carmen Diéguez10, Patricia Elizabeth Garcia10, Aurélien Dommergue11,12, Helene Angot11,12, Olivier Magand12,11, Henrik Skov13, Milena Horvat14, Jože Kotnik14, Katie Alana Read15, Luis Mendes Neves16, Bernd Manfred Gawlik17, Fabrizio Sena17, Nikolay Mashyanov18, Vladimir Obolkin19, Dennis Wip20, Xin Bin Feng21, Hui Zhang21, Xuewu Fu21, Ramesh Ramachandran22, Daniel Cossa23, Joël Knoery24, Nicolas Marusczak23, Michelle Nerentorp25, Claus Norstrom13.
Abstract
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.eu) and started in November 2010 with the overall goal to develop a coordinated global observing system to monitor Hg on a global scale, including a large network of ground-based monitoring stations, ad hoc periodic oceanographic cruises and measurement flights in the lower and upper troposphere as well as in the lower stratosphere. To date, more than 40 ground-based monitoring sites constitute the global network covering many regions where little to no observational data were available before GMOS. This work presents atmospheric Hg concentrations recorded worldwide in the framework of the GMOS project (2010-2015), analyzing Hg measurement results in terms of temporal trends, seasonality and comparability within the network. Major findings highlighted in this paper include a clear gradient of Hg concentrations between the Northern and Southern hemispheres, confirming that the gradient observed is mostly driven by local and regional sources, which can be anthropogenic, natural or a combination of both.Entities:
Year: 2016 PMID: 30245704 PMCID: PMC6145827 DOI: 10.5194/acp-16-11915-2016
Source DB: PubMed Journal: Atmos Chem Phys ISSN: 1680-7316 Impact factor: 6.133