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Mercury emissions of a coal-fired power plant in Germany
Hg ∕ SO2, Hg ∕ CO, NOx ∕ SO2 (NOx being the sum of NO and NO2) emission ratios (ERs) in the plume...
A Weigelt, F Slemr, R Ebinghaus, N Pirrone, J Bieser, J Bodewadt, G Esposito, PFJ van Velthoven | Status: published | Journal: Atm. Chem. Phys. | Volume: 16 | Year: 2016 | First page: 13653 | Last page: 13668 | doi: 10.5194/acp-16-13653-2016
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Five years of observations of ozone profiles over Lauder, New Zealand
Altitude profiles of ozone (O3) over Lauder (45°S, 170°E) performed using a lidar, ozonesondes, a...
EJ Brinksma, J Ajtic, JB Bergwerff, GE Bodecker, IS Boyd, JF de Haan, W Hogervorst, JW Hovernier, DPJ Swart | Status: published | Journal: J. Geophys. Res. | Volume: 107 | Year: 2002 | First page: 4216 | doi: 10.1029/2001JD000737
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Tropospheric mercury vertical profiles between 500 and 10 000 m in central Europe
The knowledge of the vertical distribution of atmospheric mercury (Hg) plays an important role in...
A Weigelt, R Ebinghaus, N Pirrone, J Bieser, J Bodewadt, G Esposito, F Slemr, PFJ van Velthoven, A Zahn, H Ziereis | Status: published | Journal: Atm. Chem. Phys. | Year: 2016 | First page: 4135 | Last page: 4146 | doi: 10.5194/acp-16-4135-2016
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Projection of global wave climate change towards the end of the 21st century
Wind generated waves at the sea surface are of outstanding importance for both their practical re...
A Semedo, R Weisse, A Behrens, A Sterl, L Bengtsson, H Günther | Status: published | Journal: J. Climate | Volume: 26 | Year: 2013 | First page: 8269 | Last page: 8288 | doi: 10.1175/JCLI-D-12-00658.1
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Wind Sea and Swell Waves in the Nordic Seas
The output of a high-resolution wave model of the Nordic Seas is analyzed and a climatology devel...
A Semedo, R Vettor, O Breivik, A Sterl, M Reistad, C Guedes Soares | Conference: 13th International Workshop on Wave Hindcasting and Forecasting and 4th Coastal Hazards Symposium | Organisation: GOOS | Place: Banff, Canada | Year: 2013 | doi: 10.1007/s10236-014-0788-4 | First page: 0 | Last page: 0
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