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First 1258 results for ” A Rauthe-Schöch”

1. Verification of an objective analysis scheme. Meteorological analyses and their verifcation by trajectories of radioactive air masses during the Chernobyl disaster.

   An Intermittent data assimilation scheme has been used to produce wind and precipitation flelds d...

   G.J. Cats, B.J. de Haan and L.M. Hafkenscheid | Year: 1987 | Pages: 29

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2. Description and evaluation of the tropospheric aerosol scheme in the Integrated Forecasting System (IFS-AER, cycle 47R1) of ECMWF

   This article describes the Integrated Forecasting System aerosol scheme (IFS-AER) used operationa...

   Remy S., Kipling Z., Huijnen V., Flemming J., Nabat P., Michou M., Ades M., Engelen R., Peuch V.-H. | Journal: Geoscientific Model Development | Volume: 15 (12) | Year: 2022 | First page: 4881 | Last page: 4912 | doi: 10.5194/gmd-15-4881-2022

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3. Deep convective injection of boundary layer air into the lowermost stratosphere at midlatitudes
   H Fischer, M de Reus, M Traub, J Williams, J Lelieveld, J de Gouw, C Warneke, H Schlager, A Minikin, MP Scheele, P Siegmund | Status: published | Journal: Atm. Chem. Phys. | Volume: 3 | Year: 2003 | First page: 739 | Last page: 745 | doi: http://www.copernicus.org/EGU/acp/acp/3/739

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4. Cloud detection and classification based on MAX-DOAS observations

   Multi-axis differential optical absorption spec- troscopy (MAX-DOAS) observations of aerosols and...

   T Wagner, A Apituley, S Beierle, S Dörner, U Friess, J Remmers, R Shaiganfar | Status: published | Journal: Atmospheric Measurement Techniques | Year: 2014 | First page: 1289 | Last page: 1320 | doi: 10.5194/amt-7-1289-2014

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5. SCIENTIFIC PREPARATIONS FOR AEOLUS AND AEOLUS FOLLOW-ON

   In spring 2010 the ESA Core Explorer Atmospheric Dynamics Mission, ADM-Aeolus is due for launch. ...

   ACM Stoffelen, GJ Marseille, J de Kloe, K Houchi, H Körnich, N Žagar | Conference: 9th International Winds Workshop | Organisation: NOAA | Place: Annapolis, maryland, USA | Year: 2008 | First page: 0 | Last page: 0

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