S02 - P04 - 1 ADM-Aeolus Ocean Surface Calibration and Level-2B Wind-Retrieval Processing Jos de Kloe1, Ad Stoffelen1, Gert-Jan Marseille1, David Tan2, Lars Isaksen2, Charles Desportes3, Christophe Payan3, Alain Dabas3, Dorit Huber4, Oliver Reitebuch5, Pierre Flamant6, Herbert Nett7, Olivier Le Rille7, and Anne-Grete Straume7 1Royal Dutch Meteorological Institute (KNMI), P.O. Box 201, NL 3730 AE, De Bilt, The Netherlands; email:
[email protected]; 2European Center for Medium-range Weather Forecasting (ECMWF), Shinfield Park, Reading RG2 9AX, UK; 3Met´ eo´ France, 42 avenue Coriolis, 31057 Toulouse, France; 4DorIT, Munich, Germany; 5DLR, Oberpfaffenhofen, D-82234 Wessling, Germany; 6LMD/IPSL, 91128 Palaiseau, France; 7ESA/ESTEC, Postbus 299, NL 2200 AG, Noordwijk, The Netherlands. ABSTRACT atmospheric temperature and pressure profiles (from a numerical weather prediction model) to retrieve the wind Preparations for the European Space Agency’s (ESA) profile from the spectrometer data. This software will be Atmospheric Dynamics Mission (ADM-Aeolus), which is made available by ESA as source code, free of charge, scheduled for launch in 2011, are in full progress. The to all interested users in the meteorological/research direct detection high spectral resolution Doppler Wind community, and may be used as standalone software, Lidar (DWL) satellite instrument will be the first to mea- or integrated as subroutine in a larger system for use in sure wind profiles from space, from the surface up to scientific or operational applications. The working of the 30 km altitude [1] and [2]. To achieve this, a laser at L2Bp will be illustrated at the conference. 355 nm pulsed at 100 Hz is pointed towards the at- mosphere.