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Historical wind speed equivalents of the Beaufort scale, 1850-1950
The original Beaufort scale of wind force is a scale that does not present the actual velocity wi...
H Wallbrink, FB Koek | Year: 2009
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Internal variability of the wind-driven ocean circulation
The ocean circulation is known to vary on a multitude of time and spatial scales.
Due to the larg...
CA Katsman | University: Utrecht | Year: 2001
Publication
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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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High Resolution Model Intercomparison Project (HighResMIP v1.0) for CMIP6
Robust projections and predictions of climate vari-
ability and change, particularly at regional ...
RJ Haarsma, et al. | Status: published | Journal: Geoscientific Model Development | Year: 2016 | doi: 10.5194/gmd-9-4185-2016
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