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dc.contributor.authorBerg, Torunn
dc.contributor.authorCole, AS
dc.contributor.authorEngelsen, Ola
dc.contributor.authorSteffen, A
dc.contributor.authorPfaffhuber, Katrine Aspmo
dc.date.accessioned2015-09-30T08:53:08Z
dc.date.accessioned2015-11-09T11:51:04Z
dc.date.available2015-09-30T08:53:08Z
dc.date.available2015-11-09T11:51:04Z
dc.date.issued2013
dc.identifier.citationAtmospheric Chemistry And Physics 2013, 13(13):6575-6586nb_NO
dc.identifier.issn1680-7324
dc.identifier.urihttp://hdl.handle.net/11250/2359723
dc.description.abstractResults from ten years of gaseous elemental mercury (GEM) measurements at Zeppelin station, Ny-A° lesund, Svalbard, show no overall annual trend between 2000 and 2009. Seasonal trend analysis showed significantly decreasing trends in January, February, March and June (−4.5 to −14.9 pgm−3 yr−1) and significantly increasing trends in May and July through December (1.5 to 28.7 pgm−3 yr −1). Results showed that atmospheric mercury depletion events (AMDEs) were equally distributed between April and May with only a few having been observed in March and June. A negative correlation between AMDEs and temperature is reported and supports earlier observations that AMDEs tend to occur at low temperatures. Lower concentrations of GEM were seen at lower temperatures below a threshold of 0 C. The occurrence of AMDEs and wind direction were well correlated with the lowest GEM measured when the wind direction was from the Arctic Ocean region. Wind speed was found to not correlate with AMDEs, but the lowest GEM concentrations were observed at low wind speeds between 4 and 11ms−1. AMDEs and relative humidity did not correlate well, but the lowest GEM levels appeared when the relative humidity was between 80 and 90 %. Diurnal variation was observed especially during the month of March and is probably due to daytime snow surface emission induced by solar radiation. Relationships between GEM concentration and the Northern Hemisphere climate indices were investigated to assess if these climate parameters might reflect different atmospheric conditions that enhance or reduce spring AMDE activity. No consistent pattern was observed.nb_NO
dc.language.isoengnb_NO
dc.publisherEuropean Geosciences Unionnb_NO
dc.titleTen-year trends in atmospheric mercury concentrations, meteorological effects and climate variables at Zeppelin, Ny-Ålesundnb_NO
dc.typeJournal articlenb_NO
dc.typePeer revieweden_GB
dc.date.updated2015-09-30T08:53:08Z
dc.source.pagenumber6575–6586nb_NO
dc.source.volume13nb_NO
dc.source.journalAtmospheric Chemistry And Physicsnb_NO
dc.source.issue13nb_NO
dc.identifier.doi10.5194/acp-13-6575-2013
dc.identifier.cristin1054294
dc.description.localcode© Author(s) 2013. This work is distributed under the Creative Commons Attribution 3.0 License.nb_NO


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