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First 1384 results for ” I Haddeland”

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

   Publication

2. Assessing the effects of nitrogen deposition and climate on carbon isotope discrimination and intrinsic water-use efficiency of angiosperm and conifer trees under rising CO2 conditions

   The objective of this study is to globally assess the effects of atmospheric nitrogen deposition ...

   S Leonardi, T Gentilesca, R Guerrieri, F Ripullone, F Magnani, M Mencuccini, T van Noije, M Borghetti | Status: published | Journal: Glob. Change Biol. | Volume: 18 | Year: 2012 | First page: 2925 | Last page: 2944 | doi: 10.1111/j.1365-2486.2012.02757.x

   Publication

3. 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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4. Traceability of CM-11 pyranometer calibrations at KNMI

   KNMI has used Kipp&Zonen CM-11 pyranometers for operational radiation measurements since 1989...

   T. Mathijssen, J. Bijma, W. Knap | Year: 2018 | Pages: 33

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5. 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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