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First 4988 results for ” H.W. van den Brink and I.L. Wijnant”

1. Can we explain the observed methane variability after the Mount Pinatubo eruption?

   The CH4 growth rate in the atmosphere showed large variations after the Pinatubo eruption in June...

   N Bândă, M Krol, M van Weele, T van Noije, P Le Sager, T Röckmann | Status: published | Journal: Atmos. Chem. Phys. | Volume: 16 | Year: 2016 | First page: 195 | Last page: 214 | doi: 10.5194/acp-16-195-2016

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2. 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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3. Downscaling HARMONIE-AROME with Large-Eddy simulation

   In this report we build on previous work by e.g. Neggers et al. (2012); Schalkwijk et al. (2015a)...

   B.J.H. van Stratum, A.P. Siebesma, J. Barkmeijer, B. van Ulft | Year: 2019 | Pages: 38

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4. Foutencontrole bij meteorologische metingen

   Foutencontrole bij meteorologische metingen

   J.J.M. van Gorp en H.M. van der Kolk | Year: 1985 | Pages: 70

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5. High sensitivity of Aeolus UV surface returns to surface reflectivity

   Global ultraviolet (UV) surface reflectivity climatologies are all composed from daylight passive...

   L. D. Labzovskii, G. J. van Zadelhoff, L. G. Tilstra, J. de Kloe, D. P. Donovan & A. Stoffelen | Journal: Nature scientific reports | Volume: 13 | Year: 2023 | First page: 17552 | doi: 10.1038/s41598-023-44525-5

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