the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Monitoring sudden stratospheric warmings under climate change since 1980 based on reanalysis data verified by radio occultation
Ying Li
Gottfried Kirchengast
Marc Schwaerz
Yunbin Yuan
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This study retrieves RO observations from the FY‑3E satellite using 1‑s undifferenced LEO clock corrections. Results are compared against those from 30‑s undifferenced and single‑difference approaches. The 1‑s clock corrections outperform the other two schemes, yielding the greatest improvement in bending‑angle profiles within the 40–60 km altitude range. These findings support future operational processing and archive reprocessing of all Fengyun GNSS occultation datasets.
This study retrieves RO observations from the FY‑3E satellite using 1‑s undifferenced LEO clock corrections. Results are compared against those from 30‑s undifferenced and single‑difference approaches. The 1‑s clock corrections outperform the other two schemes, yielding the greatest improvement in bending‑angle profiles within the 40–60 km altitude range. These findings support future operational processing and archive reprocessing of all Fengyun GNSS occultation datasets.
We investigated the potential of radio occultation (RO) data for climate-oriented wind field monitoring, focusing on the equatorial band within ±5° latitude. In this region, the geostrophic balance breaks down, and the equatorial balance approximation takes over. The study encourages the use of RO wind fields for mesoscale climate monitoring for the equatorial region, showing a small improvement in the troposphere when including the meridional wind in the zonal-mean total wind speed.