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First 2149 results for ” AP Stroeven”

1. What controls the vertical distribution of aerosol? Relationships between process sensitivity in HadGEM3–UKCA and inter-model variation from AeroCom Phase II

   The vertical profile of aerosol is important for its radiative effects, but weakly constrained by...

   Z Kipling, P Stier, CE Johnson, GW Mann, N Bellouin, SE Bauer, T Bergman, M Chin, T Diehl, SJ Ghan, T Iversen, A Kirkevåg, H Kokkola, X Liu, G Luo, T van Noije, KJ Pringle, K von Salzen, M Schulz, Ø Seland, RB Skeie, T Takemura, K Tsigaridis, K Zhang | Status: published | Journal: Atmos. Chem. Phys. | Volume: 16 | Year: 2016 | First page: 2221 | Last page: 2241 | doi: 10.5194/acp-16-2221-2016

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2. 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

3. Samenvatting voor beleidsmakers Intergovernmental Panel for Climate Change (IPCC), vijfde assessment cyclus, Werkgroep I

   De bijdrage van Werkgroep I aan het Vijfde Assessment Rapport (AR5) van het IPCC beschouwt nieuw...

   IPCC (2013), vertaald door KNMI in 2014 | Year: 2014 | Pages: 35

   Publication

4. De toestand van het klimaat in Nederland 1999

   Dit rapport De toestand van het klimaat in Nederland 1999 is de derde van onze driejaarlijkse kl...

   GP Können, TA Buishand, T Brandsma, JJ Beersma | Year: 1999

   Publication

5. The Cabauw In-situ Observational Program 2000 - Present: Instruments, Calibrations and Set-up

   The Cabauw observational program on land surface-atmosphere interaction aims at monitoring the ph...

   F.C. Bosveld | Year: 2020 | Pages: 79

   Publication