THE ATMOSPHERIC DYNAMICS MISSION FOR GLOBAL WIND FIELD MEASUREMENT

Ad Stoffelen
Search for other papers by Ad Stoffelen in
Current site
Google Scholar
PubMed
Close
,
Jean Pailleux
Search for other papers by Jean Pailleux in
Current site
Google Scholar
PubMed
Close
,
Erland Källén
Search for other papers by Erland Källén in
Current site
Google Scholar
PubMed
Close
,
J. Michael Vaughan
Search for other papers by J. Michael Vaughan in
Current site
Google Scholar
PubMed
Close
,
Lars Isaksen
Search for other papers by Lars Isaksen in
Current site
Google Scholar
PubMed
Close
,
Pierre Flamant
Search for other papers by Pierre Flamant in
Current site
Google Scholar
PubMed
Close
,
Werner Wergen
Search for other papers by Werner Wergen in
Current site
Google Scholar
PubMed
Close
,
Erik Andersson
Search for other papers by Erik Andersson in
Current site
Google Scholar
PubMed
Close
,
Harald Schyberg
Search for other papers by Harald Schyberg in
Current site
Google Scholar
PubMed
Close
,
Alain Culoma
Search for other papers by Alain Culoma in
Current site
Google Scholar
PubMed
Close
,
Roland Meynart
Search for other papers by Roland Meynart in
Current site
Google Scholar
PubMed
Close
,
Martin Endemann
Search for other papers by Martin Endemann in
Current site
Google Scholar
PubMed
Close
, and
Paul Ingmann
Search for other papers by Paul Ingmann in
Current site
Google Scholar
PubMed
Close
Full access

The prime aim of the Atmospheric Dynamics Mission is to demonstrate measurements of vertical wind profiles from space. Extensive studies conducted by the European Space Agency over the past 15 years have culminated in the selection of a high-performance Doppler wind lidar based on direct-detection interferometric techniques. Such a system, with a pulsed laser operating at 355-nm wavelength, would utilize both Rayleigh scattering from molecules and Mie scattering from thin cloud and aerosol particles; measurement of the residual Doppler shift from successive levels in the atmosphere provides the vertical wind profiles. The lidar would be accommodated on a satellite flying in a sun-synchronous orbit, at an altitude of ~400 km, providing near-global coverage; target date for launch is in 2007. Processing of the backscatter signals will provide about 3000 globally distributed wind profiles per day, above thick clouds or down to the surface in clear air, at typically 200-km separation along the satellite track. Such improved knowledge of the global wind field is crucial to many aspects of climate research and weather prediction. Knowledge over large parts of the Tropics and major oceans is presently quite incomplete—leading to major difficulties in studying key processes in the climate system and in improving numerical simulations and predictions; progress in climate modeling is indeed intimately linked to progress in numerical weather prediction. The background studies, potential impact on climate and weather prediction, choice of measurement specifications, and the lidar technology are discussed.

Royal Dutch Meteorological Institute (KNMI), De Bilt, Netherlands

Méteó-France, Toulouse, France

Meteorological Institute of the University of Stockholm, Stockholm, Sweden

Microwave Management Associates, Marlow, Bucks, United Kingdom

European Centre for Medium-Range Weather Forecasts, Reading, United Kingdom

Laboratoire Meteorologique Dynamique, CNRS, Palaiseau, France

Deutscher Wetterdienst (DWD), Offenbach, Germany

Meteorologisk Institutt, Oslo, Norway

European Space Research and Technology Centre (ESTEC), Noordwijk, Netherlands

CORRESPONDING AUTHOR: Paul Ingmann, Directorate of Earth Observation Programmes, ESA/ESTEC, Mail Code EOP-SMA, NL-2200 AG Noordwijk, Netherlands, E-mail: paul.ingmann@esa.int

The prime aim of the Atmospheric Dynamics Mission is to demonstrate measurements of vertical wind profiles from space. Extensive studies conducted by the European Space Agency over the past 15 years have culminated in the selection of a high-performance Doppler wind lidar based on direct-detection interferometric techniques. Such a system, with a pulsed laser operating at 355-nm wavelength, would utilize both Rayleigh scattering from molecules and Mie scattering from thin cloud and aerosol particles; measurement of the residual Doppler shift from successive levels in the atmosphere provides the vertical wind profiles. The lidar would be accommodated on a satellite flying in a sun-synchronous orbit, at an altitude of ~400 km, providing near-global coverage; target date for launch is in 2007. Processing of the backscatter signals will provide about 3000 globally distributed wind profiles per day, above thick clouds or down to the surface in clear air, at typically 200-km separation along the satellite track. Such improved knowledge of the global wind field is crucial to many aspects of climate research and weather prediction. Knowledge over large parts of the Tropics and major oceans is presently quite incomplete—leading to major difficulties in studying key processes in the climate system and in improving numerical simulations and predictions; progress in climate modeling is indeed intimately linked to progress in numerical weather prediction. The background studies, potential impact on climate and weather prediction, choice of measurement specifications, and the lidar technology are discussed.

Royal Dutch Meteorological Institute (KNMI), De Bilt, Netherlands

Méteó-France, Toulouse, France

Meteorological Institute of the University of Stockholm, Stockholm, Sweden

Microwave Management Associates, Marlow, Bucks, United Kingdom

European Centre for Medium-Range Weather Forecasts, Reading, United Kingdom

Laboratoire Meteorologique Dynamique, CNRS, Palaiseau, France

Deutscher Wetterdienst (DWD), Offenbach, Germany

Meteorologisk Institutt, Oslo, Norway

European Space Research and Technology Centre (ESTEC), Noordwijk, Netherlands

CORRESPONDING AUTHOR: Paul Ingmann, Directorate of Earth Observation Programmes, ESA/ESTEC, Mail Code EOP-SMA, NL-2200 AG Noordwijk, Netherlands, E-mail: paul.ingmann@esa.int
Save