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Rainfall Generator for the Rhine Basin: Sensitivity to the composition of the feature vector and passive simulations
Since the mid 1990s rainfall generators for the Rhine and Meuse basins have been developed. These...
Jules Beersma | Year: 2011 | Pages: 18
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A climatology of infrasound observations at the ARCI array in Norway
Infrasound was first discovered after the violent eruption of the Krakatoa, Indonesia, in 1883. L...
LG Evers, J Schweitzer | Year: 2009
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Recurrence intervals for the closure of the Dutch Maeslant surge barrier
The Dutch Maeslant Barrier, a movable surge barrier in the mouth of the river Rhine, closes when ...
HW van den Brink, S de Goederen | Status: published | Journal: Ocean Science | Volume: 13 | Year: 2017 | First page: 691 | Last page: 701 | doi: 10.5194/os-13-691-2017
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Analysis of global methane changes after the 1991 Pinatubo volcanic eruption
The global methane (CH4) growth rate showed large variations after the eruption of Mount Pinatubo...
N Bândă, M Krol, M van Weele, TPC van Noije, T Röckmann | Status: published | Journal: Atmos. Chem. Phys. | Volume: 13 | Year: 2013 | First page: 2267 | Last page: 2281 | doi: 10.5194/acp-13-2267-2013
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Wind Tunnel and Field Test of Three 2D Sonic Anemometers
The Royal Netherlands Meteorological Institute (KNMI) uses conventional cup anemometers and wind ...
Wiel Wauben | Year: 2007 | Pages: 166
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