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A probabilistic approach for SeaWinds data assimilation: an improvement in the nadir region
Scatterometer sea-surface wind observations are being successfully assimilated into Numerical Wea...
M Portabella, A Stoffelen | Year: 2002
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Extreme hydro-meteorological events and their probabilities
Extreme hydro-meteorological events usually have a large impact on our society. For safety standa...
JJ Beersma | University: Wageningen Universiteit | Year: 2007
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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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How big is an OMI pixel?
The Ozone Monitoring Instrument (OMI) is a
push-broom imaging spectrometer, observing solar...
M de Graaf, H Sihler, LG Tilstra, P Stammes | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 9 | Year: 2016 | First page: 3607 | Last page: 3618 | doi: 10.5194/amt-9-3607-2016
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Representativeness errors in comparing chemistry transport and chemistry climate models with satellite UV–Vis tropospheric column retrievals
Ultraviolet–visible (UV–Vis) satellite retrievals of trace gas columns of nitrogen dioxide (NO2),...
KF Boersma, GCM Vinken, HJ Eskes | Status: published | Journal: Geoscientific Model Development | Year: 2016 | First page: 875 | Last page: 898 | doi: 10.5194/gmd-9-875-2016
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