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First 4364 results for ” Wilco Hazeleger and Sybren Drijfhout”

1. Pathfinder: Applying graph theory for consistent tracking of daytime mixed layer height with backscatter lidar

   The height of the atmospheric boundary layer or mixing layer is an important parameter for unders...

   M de Bruine, A Apituley, , DP Donovan, H Klein Baltink | Status: submitted | Journal: Atmospheric Measurement Techniques | Year: 2017 | doi: doi:10.5194/amt-2016-327

   Publication

2. The impact of the ozone effective temperature on satellite validation using the Dobson spectrophotometer network

   The main aim of the paper is to demonstrate an approach for post-processing of the Dobson spectro...

   ME Koukouli, M Zara, C Lerot, K Fragkos, D Balis, M Van Roozendael, MAF Allaart, RJ van der A | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 9 | Year: 2016 | First page: 2055 | Last page: 2065 | doi: 10.5194/amt-9-2055-2016

   Publication

3. On the Mechanism of North Atlantic Decadal Variability

   North Atlantic decadal climate variability is studied with a coupled atmosphere–ocean–sea ice mod...

   FM Selten, RJ Haarsma, JD Opsteegh | Status: published | Journal: J. Climate | Volume: 12 | Year: 1999 | First page: 1956 | Last page: 1973

   Publication

4. Full-year evaluation of nonmeteorological echo removal with dual-polarization fuzzy logic for two C-band radars in a temperate climate

   The Royal Netherlands Meteorological Institute (KNMI) operates two dual-polarization C-band weath...

   A Overeem, R Uijlenhoet, H Leijnse | Status: published | Journal: J. Atm. Oceanic Technol. | Volume: 37 | Year: 2020 | First page: 1643 | Last page: 1660 | doi: 10.1175/JTECH-D-19-0149.1

   Publication

5. A Reappraisal of the Thermal Growing Season Length across Europe

   Growing season length (GSL) indices derived from surface air temperature are frequently used in c...

   RC Cornes, G van der Schrier, AA Squintu | Status: published | Journal: Int. J. Climatology | Year: 2018 | doi: doi:10.1002/joc.5913

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