Evidence date30 Sept 2026
AreasP02
OutcomeObserved in real data
●   How we do it / Result

Telling apart what caused a measurement offset, rechecked on a like-for-like basis

Question

When readings of the same reference site disagree, which candidate causes (instrument, viewing geometry and ground-surface effects, atmosphere, or a mismatch in what area was compared) are responsible at each site, and do the earlier answers survive once surface readings are compared with surface truth?

Observed in real data How stages are defined

§ 01
The result

What we did

An earlier entry in this research area attributed measurement offsets site by site. Part of the evidence behind it compared surface readings with top-of-atmosphere reference values, a mismatch found and fixed in September. This entry rechecks those attributions with surface readings compared against measured surface truth, and adds three new real-data analyses at the same reference sites.

The first rereads the site-by-site evidence on the corrected basis. The second tests whether the offsets follow viewing geometry, using real per-site sun and view angles for each acquisition at six sites. The third runs the reference sites' own measured surface and atmosphere through an independent physics calculation to test whether the atmosphere could explain the offsets.

What we saw

The earlier attributions survive the correction. At LCFR, the step between the two viewing directions is still present on the surface basis, and a fixed detector offset is still ruled out as its only cause. At RVUS, the same question is still open. At BTCN, the mismatch between the small reference target and the much larger area the satellite reading covers is confirmed on the corrected basis.

Viewing geometry is a real effect at more than one site: clearly at RVUS and LCFR, with the same sign but too weakly to be conclusive at BSCN. One shared strength describes it across those sites. In the near-infrared it accounts for the step between viewing directions at RVUS (about seven percent) and largely explains LCFR's offset. It explains only a minority of RVUS's overall offset, and none of GSCN's, where the satellite looks almost straight down.

That leaves an offset of about five percent at RVUS and GSCN that does not depend on geometry. It is not a sensor calibration error: GONA, observed by the same satellites and the same detector, reads close to zero.

The atmosphere does not explain the RVUS offset: its viewing-angle part is too small, and the atmospheric state accounts for only a few percent of the offset there. At GSCN the atmospheric state cannot yet be ruled out.

What it means

Correcting the reference basis did not overturn the earlier site-by-site findings, and the new evidence narrows them further. Viewing geometry is now seen at more than one site, though the result is still preliminary. The sensor and the atmosphere are ruled out as the cause of the largest remaining offset at RVUS. What is left is a smaller, sharper question: at RVUS, is the remaining difference in the reference measurement itself or in the area being compared, and at GSCN, could the atmospheric state also play a part? That is the next step in this research area.

§ 02
Conditions and limits
  • The register classifies these results as preliminary. Sample sizes are small: between five and about twenty dates per site depending on the analysis, and one viewing direction only at GSCN.
  • The geometry analysis can identify one combined viewing-geometry term, not separate surface and atmospheric contributions to it, and the per-site remainders depend on the shape assumed for that term.
  • The atmospheric check treats the ground as reflecting equally in all directions. Within that model the viewing-angle part of the atmospheric path is ruled out at RVUS and GSCN; the atmospheric state itself is ruled out as the main cause at RVUS but not at GSCN.
  • At RVUS, a fixed detector offset still cannot be separated from a surface-dependent effect as the cause of the step between its two viewing directions, because no other site in the data set shares its detector pairing.
  • The remaining offset of about five percent at RVUS and GSCN is not explained by the sensor. Whether it comes from the reference measurement itself or from the area compared is not yet settled, and at GSCN the atmospheric state is also still a candidate.
  • No single, site-independent treatment is justified by this evidence, and none has been applied to delivered results.
§ 03
Data and credits
  • RadCalNet RadCalNet reference measurements, with citation to Bouvet et al. 2019, Remote Sensing 11(20), 2401.
  • Copernicus Sentinel-2 Contains modified Copernicus Sentinel data 2024-2025.
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