Special Issue "Atmospheric Mercury"
A special issue of Atmosphere (ISSN 2073-4433).
Deadline for manuscript submissions: closed (30 June 2014)
Prof. Dr. Robert W. Talbot
Institute for Climate and Atmospheric Science, Department of Earth & Atmospheric Sciences, Science & Research Bldg. 1, University of Houston, Houston, TX 77204, USA
Phone: +1 713 893 1670
Interests: regional and global cycling of atmospheric mercury; distribution, composition and chemistry of reactive odd-nitrogen in the Earth's atmosphere; intercontinental transport of trace gases and aerosols; regional tropospheric chemistry and climate change in New England; climate-air quality connections; biosphere-atmosphere exchange of trace gases; development of advanced instrumentation for the measurement of reactive trace gases and aerosols
Mercury is a serious environmental toxin that is distributed globally by large-scale atmospheric circulations. Atmospheric chemists have only been studying mercury in earnest for approximately the past 10 years. In the troposphere elemental mercury (Hgo) is observed ubiquitously with contemporary mixing ratios at the parts per quadrillion by volume (ppqv; 1 ng m−3 = 112 ppqv) level. The distributions of gaseous oxidized mercury (GOM) and particulate mercury (HgP) are not well documented at this time. In fact, the chemical composition of GOM is presently highly uncertain. At most mid-latitude locations, Hgo exhibits seasonality with the lowest mixing ratios in the fall and the greatest in late winter/early spring. It is highly desirable to conduct measurements of a variety of trace gases along with atmospheric mercury to facilitate source identification, but few studies have done so to date. A serious drawback in modeling atmospheric mercury is a lack of reliable rigorous emission inventories. Consequently, much work is needed to identify mercury sources and to quantify emission strengths.
There are few published papers on measurements of atmospheric mercury from aircraft. Initial work has shown that there is little to no Hgo above the tropopause and that HgP is elevated there. The chemical cycling and transformations in the tropopause region are essentially unstudied. Both measurements and modeling are required to ascertain the important processes affecting atmospheric mercury in the tropopause region.
Manuscripts on all aspects of atmospheric mercury are welcome for this special issue.
Prof. Dr. Robert W. Talbot
Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. Papers will be published continuously (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.
Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are refereed through a peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Atmosphere is an international peer-reviewed Open Access monthly journal published by MDPI.
- elemental mercury
- gaseous oxidized mercury
- particulate mercury
- chemical transformations of atmospheric mercury
- cycling of atmospheric mercury
- regional and global modeling of atmospheric mercury
- emission inventories for atmospheric mercury