Wind Profile Satellite Observation Requirements and Capabilities

Author:

Benedetti Angela1,Borde Régis2,Dabas Alain3,Flamant Pierre4,Forsythe Mary5,Hardesty Mike6,Isaksen Lars1,Källén Erland7,Körnich Heiner7,Lee Tsengdar8,Reitebuch Oliver9,Rennie Michael1,Riishøjgaard Lars-Peter10,Schyberg Harald11,Straume Anne Grete12,Vaughan Michael13

Affiliation:

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

2. European Organisation for the Exploitation of Meteorological Satellites, Darmstadt, Germany

3. Centre National de Recherches Météorologiques, Météo France, Toulouse, France

4. Institut Pierre Simon Laplace, Paris, France

5. Met Office, Exeter, United Kingdom

6. National Oceanic and Atmospheric Administration, Boulder, Colorado

7. Department of Meteorology, Stockholm University (MISU), Stockholm, Sweden

8. NASA Science Mission Directorate, Washington, D.C.

9. Deutsches Zentrum für Luft- und Raumfahrt, Oberpfaffenhofen, Germany

10. World Meteorological Organization, Geneva, Switzerland

11. Norwegian Meteorological Institute, Oslo, Norway

12. European Space Research and Technology Centre, Noordwijk, Netherlands

13. Lidar and Optics Associates (OLA), Malvern, United Kingdom

Abstract

AbstractThe Aeolus mission objectives are to improve numerical weather prediction (NWP) and enhance the understanding and modeling of atmospheric dynamics on global and regional scale. Given the first successes of Aeolus in NWP, it is time to look forward to future vertical wind profiling capability to fulfill the rolling requirements in operational meteorology. Requirements for wind profiles and information on vertical wind shear are constantly evolving. The need for high-quality wind and profile information to capture and initialize small-amplitude, fast-evolving, and mesoscale dynamical structures increases, as the resolution of global NWP improved well into the 3D turbulence regime on horizontal scales smaller than 500 km. In addition, advanced requirements to describe the transport and dispersion of atmospheric constituents and better depict the circulation on climate scales are well recognized. Direct wind profile observations over the oceans, tropics, and Southern Hemisphere are not provided by the current global observing system. Looking to the future, most other wind observation techniques rely on cloud or regions of water vapor and are necessarily restricted in coverage. Therefore, after its full demonstration, an operational Aeolus-like follow-on mission obtaining globally distributed wind profiles in clear air by exploiting molecular scattering remains unique.

Publisher

American Meteorological Society

Subject

Atmospheric Science

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