Abstract

The long-term stability of microwave radiometers (MWR) on-board altimetry missions is critical to reduce the uncertainty on the global mean sea level estimate. Harmonization and homogenization steps are applied to MWR observations in that perspective. The Sentinel-3 tandem phase provides a unique opportunity to quantify the uncertainties on the “zero-bias line” homogenization approach defined by Bennartz et al. (2020). Initially developed to improve the performance of the wet tropospheric correction retrieval, it is used here to provide a common reference for the inter-calibration between Sentinel-3A and Sentinel-3B MWR. A simplified version of the “zero-bias line” approach, a linear correction depending on brightness temperatures, allows to strongly reduce the bias between the two radiometers for both channels (about 0.5 K) and the standard deviation of the difference (0.3 K). The full version of the approach adding a dependency on wind speed has improved the quality of the WTC retrieval (Bennartz et al. 2020) but degrades the performance of the homogenization. It is thus recommended to apply the simplified version of this approach in the processing of fundamental data record. The quantification of the uncertainties on the homogenization approach is only possible due to the ideal configuration of the Sentinel-3 tandem phase. The same dataset and the same metrics could be used to assess other approaches.

Highlights

  • The Sentinel-3 Microwave Radiometer (S3 microwave radiometers (MWR)) is a two-channels noise injection microwave radiometer

  • The stability of the wet tropospheric correction is a critical aspect of the characterization of the global mean sea level (GMSL) rise: any artificial trend on the Wet Tropospheric Correction (WTC) has a direct impact the quality of Remote Sens. 2020, 12, 3154 the GMSL

  • Such potentially land-contaminated pixels are excluded from the analysis presented by rejecting any observation less than at least 100 km offshore

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Summary

MWR Instruments On-Board Sentinel-3A and Sentinel-3B

The Sentinel-3 Microwave Radiometer (S3 MWR) (see Figure 1) is a two-channels noise injection microwave radiometer. Following the heritage of ERS-1, ERS-2 and Envisat, it operates at 23.8 GHz to observe atmospheric water vapour and at 36.5 GHz to record the presence of atmospheric liquid water. By using feed horns that are not directly on the boresight of the antenna, the 24 km diameter footprint at 23.8 GHz is located 28 km in front of the sub-satellite point and the 18.5 km diameter footprint at 36.5 GHz is located 27 km behind. MWR brightness temperatures (TB) are used to infer the amount of water vapour and liquid water in the sub-satellite atmospheric column, and to subsequently calculate the Wet Tropospheric Correction (WTC), i.e. the correction to the range, and the atmospheric attenuation (correction to the altimeter backscattering coefficient, σ0) to support altimetry observations.

Harmonization and Homogenization and the Sentinel-3 Tandem Phase
The Tandem Phase Dataset and Editing
The “Zero-Bias Line” Homogenization Method
Assessment Using S3-A and S3-B Tandem Phase
Findings
Conclusions and Recommendation for Future Missions
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