Skip to main content
Dryad

Data from: NWCSAF high resolution winds (NWCSAF GEO-I HRW) stereo AMVs over the Atlantic Ocean

Data files

Sep 11, 2026 version files 1.88 GB

Click names to download individual files

Abstract

The “stereo height assignment method” developed for NASA and NOAA for GOES-R/ABI Atmospheric Motion Vectors (AMVs), a purely geometric method based on the parallax displacement observed by two different satellites, has been included in the NWCSAF geostationary AMV product (NWCSAF GEO-I HRW, High Resolution Winds) as an extension to its v2025 code, as an additional height assignment option for AMVs in the region jointly observed by MTG-I1 and GOES-East over the Atlantic Ocean. 

A comparison has also taken place, based on ECMWF ERA5 reanalysis winds and EarthCARE Mie Attenuated Backscatter (MAB) cloud height, against the alternative height assignment method in the HRW algorithm: “Cross Correlation Contribution (CCC)”, based on the output of several NWCSAF GEO-I Cloud products (Cloud type, Cloud top temperature and height, Cloud microphysics) and with direct or indirect dependence on up to 16 NWP forecast variables.

Considering the EarthCARE MAB, for low-level clouds (< 2 km), both stereo and non-stereo heights appear to conform well with the visually identifiable cloud tops, although there are many places where the result is also ambiguous. For higher clouds, clear differences are certainly seen between stereo and non-stereo heights. Considering ECMWF ERA5 reanalysis winds, the most pronounced distinctions emerge also at high levels (> 6 km), where the mean biases of stereo and non-stereo AMVs remain similar, but the standard deviations generally favor the stereo method, reflecting improved precision in the upper-tropospheric flow where the parallax signal is strongest. 

The updated HRW algorithm will be released to NWCSAF users in 2027 inside the following software package version (NWCSAF GEO-I v2027).