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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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Coupled sea surface-atmospheric model 2. Spectrum of short wind waves
A physical model of the short wind wave spectrum in
the wavelength range from a few millimeters ...
VN Kudryavtsev, VK Makin, B Chapron | Status: published | Journal: J. Geophys. Res. | Volume: 104 | Year: 1999 | First page: 7625 | Last page: 7639
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The 2018 fire season in North America as seen by TROPOMI: aerosol layer height validation and evaluation of model-derived plume heights
Before the launch of the TROPOspheric Moni- toring Instrument (TROPOMI), only two other satellite...
G Griffin, C Sioris, J Chen, N Dickson, A Kovachik, M de Graaf, S Nanda, JP Veefkind, E Dammers, CA McLinden, P Makar | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 13 | Year: 2020 | First page: 1427 | Last page: 1445 | doi: 10.5194/amt-13-1427-2020
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KNMI contribution to the WMO Laboratory Intercomparison of Rainfall Intensity Gauges
The Commission for Instruments and Methods of Observation (CIMO-XII Casablanca, 1998) of the Worl...
W. Wauben | Year: 2006 | Pages: 174
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Cloud masking using MSG and HIRLAM
Clouds occurrence is the direct consequence of atmospheric processes relevant to the (scientific)...
J.P.J.M.M. de Valk | Year: 2006 | Pages: 58
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