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First 2415 results for ” G.D.G Folkers en A.T.F Grooters”

1. The GABLS Third Intercomparison Case for Boundary Layer Model Evaluation Part B: Results and Process Understanding

   This study describes and analyzes the results of the third GEWEX Atmospheric Boundary Layer Studi...

   FC Bosveld, P Baas, GJ Steeneveld, AAM Holtslag, WM Angevine, E Bazile, EIF de Bruijn, D Deacu, JM Edwards, M Ek, VE Larson, JE Pleim, M Raschendorfer, G Svensson | Status: published | Journal: Bound.-Layer Meteorol. | Volume: 152 | Year: 2014 | First page: 157 | Last page: 187 | doi: 10.1007/s10546-014-9919-1

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2. Characteristics of the raindrop distributions in RICO shallow cumulus

   The physical properties of rain spectra are gener- ally modeled using an analytical distribution....

   O Geoffroy, AP Siebesma, F Burnet | Status: published | Journal: Atm. Chem. Phys. | Volume: 14 | Year: 2014 | First page: 10897 | Last page: 10909 | doi: doi:10.5194/acp-14-10897-2014

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3. Observation Representativeness Error

   NWP models simulate the atmospheric state on a given model grid, thereby principally limiting the...

   GJ Marseille, A Stoffelen | Year: 2012

   Publication

4. Past changes in the vertical distribution of ozone – Part 1: Measurement techniques, uncertainties and availability

   Peak stratospheric chlorofluorocarbon (CFC) and other ozone depleting substance (ODS) concentrati...

   B Hassler, I Petropavlovskikh, J Staehelin, PF Levelt, RJ van der A, JP Veeflind, et al. | Status: published | Journal: Atmospheric Measurement Techniques | Year: 2014 | First page: 1395 | Last page: 1427 | doi: 10.5194/amt-7-1395-2014

   Publication

5. 3D Exploration of Weather Data in Combination with IASI L2 Products for Better Understanding of Potential Applications

   At the Royal Netherlands Meteorological Institute (KNMI) the Weather3DeXplorer (W3DX) is develope...

   M Koutek, S de Haan, I van der Neut, F Debie, P de Valk, S Tjemkes | Conference: EUMETSAT Meteorological Satellite Conference | Year: 2014 | First page: 0 | Last page: 0

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