Versions Compared

Key

  • This line was added.
  • This line was removed.
  • Formatting was changed.


Image AddedImage Added

Image Added

Example of Aeolus Rayleigh-clear Level-2B HLOS winds

Image RemovedImage Removed

ADM-

ADM-Aeolus (or Aeolus for short) is Aeolus was the fifth planned satellite in the Living Planet Programme of the European Space Agency after being launched on 22 August 2018. The mission's objective is to provide profiles of high-quality wind observations from the surface to around 30 km altitudethe lower stratosphere, using a Doppler wind lidar (DWL) instrument (known as ALADIN) in a near-polar sun-synchronous, dawn-dusk orbit (at around 320 km altitude). The wind information is the horizontal line-of-sight (HLOS) component, in the direction perpendicular to the satellite's velocity. The mission is intended to have a surpassed its minimum lifetime of three years (lasting nearly five years) after de-orbiting on 28 July 2023.

ECMWF is contracted by ESA to develop, in collaboration with KNMI, DLR and other partners of the Aeolus DISC the Aeolus Level 2B/C (L2B/C) processing software i.e. the wind retrieval.   The L2B wind retrieval algorithms have also been developed in the past in collaboration with Météo-France, DLR and LMD/IPSL.  ECMWF will also generate the L2B products operationally at ECMWF, ECMWF generated the NRT L2B products during the mission lifetime via the L2/Met PF (Level-2/Meteorological Processing Facility; a part of the mission's Ground Segment). The products were disseminated to ESA for further distribution to users. ECMWF also convert the L2B Earth Explorer format products to a WMO approved BUFR format and forwarded them to EUMETSAT for further distribution to the NWP/research community via the GTS and EUMETCast.

ECMWF operationally assimilated the Aeolus L2B wind observations and provide the products to ESA for further distribution.  ECMWF intend to assimilate the L2B winds in ECMWF's global NWP (Numerical Weather Prediction) model if demonstrated from 9 January 2020 to 30 April 2023. The L2B winds were proven to improve forecast skill and operational assimilation was justified, despite being a demonstration mission. Aeolus winds have a positive impact on analysis and forecast quality, particularly in the tropics and polar areas, particularly where conventional wind profiles are absent. The intention is to hopefully use reprocessed datasets in future ECMWF produced reanalyses.

Given that .  Since ALADIN is a High Spectral Resolution Lidar; then , it is also possible to derive information useful for on atmospheric composition modelling.  Aeolus will also provide information on the atmosphere's : cloud and aerosol optical properties (particle backscatter and extinction coefficients, via the Level-2A product).   ECMWF has contributed to ESA funded observation impact studies to assess the potential impact of the Aeolus data in the past. We expect the Aeolus mission to have a positive impact on analysis and forecast quality, in particular the improvement of winds in the tropics.

More information is available at ESA's website.

Aeolus is expected to be launched in December 2017; this website provides

This is also being researched at ECMWF for the benefit of the CAMS model.

Further information and publications on Aeolus:

will take

The L2B processing software

KNMI and ECMWF and KNMI develop the ADM- Aeolus Level-2B wind retrieval software, the main output of which produces HLOS winds are HLOS wind observations, which are suitable for use in NWP and meteorological research.   The algorithms are described in Tan et al. (Tellus, A, 2008, 60, 2, 191-205), however note that there have been many modifications to the software since the reference was written (the Algorithm Theoretical Baseline document is up-to-date; see link Refer to the Algorithm Theoretical Basis document for information about the algorithms (see documentation links below).

Downloading the L2B processing software and documentation

  • The ADM- Aeolus Level-2B/C processing documentation v2.30 (including the Software Release Note, the Algorithm Theoretical Baseline Basis and the Input/Output Data Definitions Interface Control documents) and associated datasets (needed to test the success of the installation) is available for download:
    Button Hyperlink
    titleDownload Aeolus L2B/C documentation and datasets
    typestandard
    urlDocumentation L2B processor documentation and datasets
  • The source code (v2.30) can be freely downloaded for free from from our website (upon acceptance of the licence terms): 
    Button Hyperlink
    titleDownload Aeolus L2B processor package
    typestandard
    urlhttp://www.ecmwf.int/en/forecasts/software-and-tools/software/aeolus
  • News on updates to the software, e.g. new planned deliveries, will be is provided here
  • Technical Notes prepared for ESA regarding the L2B/C processing can be downloaded here (they are useful to help understand more about the L2B products)

Image Removed

An artist's impression of the ADM-Aeolus satellite in orbit (courtesy of ESA).

Image Removed

An example of Aeolus L2B Rayleigh-clear wind observations, generated by running the genuine ground processing (i.e. L0/L1A/L1B/L2B processing) upon a realistic simulation of the raw data (E2S).

  • Aeolus L2B winds have a WMO approved BUFR template:
    • See here for the BUFR template. Search for "Atmospheric Laser Doppler Instrument (ALADIN) L2b data", table reference = 3 40 013. 
    • The satellite identifier number is 48 for AEOLUS (see here)
    • The satellite instrument number is 130 for the ESA Lidar ALADIN Atmospheric laser Doppler instrument (see here)
  • Some guidance for NWP users on the L2B BUFR data

An example of real Aeolus L2B HLOS winds, from an orbit just to the west of hurricane Dorian on 1 September 2019:

Image Added

Image Added