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First 223 results for ” N Blond”

1. Spontaneous abrupt climate change due to atmospheric blocking-sea-ice-ocean feedback in an unforced climate model simulation
   SS Drijfhout, E Gleeson, HA Dijkstra, V Livina | Status: published | Journal: Proc. Nat. Acad. Sciences | Volume: 110 | Year: 2013 | First page: 19713 | Last page: 19718 | doi: 10.1073/pnas.1304912110

   Publication

2. Intercomparison and interpretation of single-column model simulations of a nocturnal stratocumulus-topped marine boundary layer

   Ten single-column models (SCMs) from eight groups are used to simulate a nocturnal nonprecipitati...

   P Zhu, CS Bretherton, M Kohler, A Cheng, A Chlond, Q Geng, P Austin, JC Golaz, G Lenderink, A Lock, B Stevens | Status: published | Journal: Mon. Wea. Rev. | Volume: 133 | Year: 2005 | First page: 2741 | Last page: 2758 | doi: doi: 10.1175/MWR2997.1

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3. A single-column model intercomparison of a heavily drizzling stratocumulus topped boundary layer

   This study presents an intercomparison of single-column model simulations of a nocturnal heavily ...

   MC Wyant, CS Bretherton, A Chlond, BM Griffin, H Kitagawa, CL Lappen, VE Larson, A Lock, S Park, SR de Roode, M Zhao, AS Ackerman | Status: published | Journal: J. Geophys. Res. | Volume: 112 | Year: 2007 | doi: 10.1029/2007JD008536

   Publication

4. Humidity sensors for land and maritime stations

   In order to find a suitable humidity sensor for the KNMI measuring network, a set of five differe...

   HI Bloemink | Conference: WMO Technical Conference on Meteorological and Environmental Instruments and Methods of Observation | Organisation: WMO | Place: St. Petersburg, Russia | Year: 2008 | First page: 0 | Last page: 0

   Publication

5. KNMI Visibility Standard for Calibration of Scatterometers

   Scatterometers are used to measure visibility, but their calibration is not trivial. Calibration ...

   HI Bloemink | Conference: WMO Technical Conference on | Organisation: WMO | Place: Geneva, Switzerland | Year: 2006 | First page: 0 | Last page: 0

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