Ten-year trends in atmospheric mercury concentrations, meteorological effects and climate variables at Zeppelin, Ny-Ålesund

Results from ten years of gaseous elemental mercury (GEM) measurements at Zeppelin station, Ny-Ålesund, 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 pg m<sup>&...

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Main Authors: T. Berg, K. A. Pfaffhuber, A. S. Cole, O. Engelsen, A. Steffen
Format: Article
Language:English
Published: Copernicus Publications 2013-07-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/6575/2013/acp-13-6575-2013.pdf
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author T. Berg
K. A. Pfaffhuber
A. S. Cole
O. Engelsen
A. Steffen
author_facet T. Berg
K. A. Pfaffhuber
A. S. Cole
O. Engelsen
A. Steffen
author_sort T. Berg
collection DOAJ
description Results from ten years of gaseous elemental mercury (GEM) measurements at Zeppelin station, Ny-Ålesund, 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 pg m<sup>&minus;3</sup> yr<sup>&minus;1</sup>) and significantly increasing trends in May and July through December (1.5 to 28.7 pg m<sup>&minus;3</sup> yr <sup>&minus;1</sup>). 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 11 m s<sup>−1</sup>. 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.
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spelling doaj.art-4eced126410e4914a6d3398b568a0dc02022-12-21T22:41:44ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-07-0113136575658610.5194/acp-13-6575-2013Ten-year trends in atmospheric mercury concentrations, meteorological effects and climate variables at Zeppelin, Ny-ÅlesundT. BergK. A. PfaffhuberA. S. ColeO. EngelsenA. SteffenResults from ten years of gaseous elemental mercury (GEM) measurements at Zeppelin station, Ny-Ålesund, 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 pg m<sup>&minus;3</sup> yr<sup>&minus;1</sup>) and significantly increasing trends in May and July through December (1.5 to 28.7 pg m<sup>&minus;3</sup> yr <sup>&minus;1</sup>). 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 11 m s<sup>−1</sup>. 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.http://www.atmos-chem-phys.net/13/6575/2013/acp-13-6575-2013.pdf
spellingShingle T. Berg
K. A. Pfaffhuber
A. S. Cole
O. Engelsen
A. Steffen
Ten-year trends in atmospheric mercury concentrations, meteorological effects and climate variables at Zeppelin, Ny-Ålesund
Atmospheric Chemistry and Physics
title Ten-year trends in atmospheric mercury concentrations, meteorological effects and climate variables at Zeppelin, Ny-Ålesund
title_full Ten-year trends in atmospheric mercury concentrations, meteorological effects and climate variables at Zeppelin, Ny-Ålesund
title_fullStr Ten-year trends in atmospheric mercury concentrations, meteorological effects and climate variables at Zeppelin, Ny-Ålesund
title_full_unstemmed Ten-year trends in atmospheric mercury concentrations, meteorological effects and climate variables at Zeppelin, Ny-Ålesund
title_short Ten-year trends in atmospheric mercury concentrations, meteorological effects and climate variables at Zeppelin, Ny-Ålesund
title_sort ten year trends in atmospheric mercury concentrations meteorological effects and climate variables at zeppelin ny alesund
url http://www.atmos-chem-phys.net/13/6575/2013/acp-13-6575-2013.pdf
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