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@ARTICLE{Yang:1045821,
author = {Yang, Peiqi and Liu, Zhigang and Han, Dalei and Zhang,
Runfei and Siegmann, Bastian and Liu, Jing and Zhao, Huarong
and Rascher, Uwe and Chen, Jing M. and van der Tol,
Christiaan},
title = {{M}itigating the black-soil problem in the
reflectance-to-fluorescence ({R}2{F}) relationship: {A}
soil-adjusted reflectance-based approach for downscaling
{SIF}},
journal = {Remote sensing of environment},
volume = {330},
issn = {0034-4257},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2025-03620},
pages = {114998 -},
year = {2025},
note = {Bitte Post-print ergänzen},
abstract = {Solar-induced chlorophyll fluorescence (SIF) is an
effective probe for photosynthesis, but this remote
sensingsignal is affected by multiple factors, including
radiation intensity, canopy structure, sun-observer
geometry, andleaf physiological status. The complex
interplay among these factors causes substantial
discrepancies among topof-canopy (TOC) SIF, leaf-level
average SIF and actual photosynthetic activity. Downscaling
TOC SIF to the leafleveland decoupling structural and
physiological information remain major challenges in the use
of SIF signalsfor remote sensing of photosynthesis. To
address these challenges, the R2F
(reflectance-to-fluorescence) theorywas developed, grounded
in the similarity in radiative transfer processes governing
SIF and reflectance. Thistheory establishes a physical
relationship between near-infrared reflectance (Rnir) and
the far-red SIF scatteringcoefficient (σF). On this basis,
SIF signals can be scaled from the canopy to the leaf level
by normalizing σF,estimated from reflectance as σF =
Rnir/i0, where i0 denotes canopy interceptance. However, the
original R2Fformulation assumes a non-reflective soil. This
simplification breaks down in sparse canopies, where soil
contributionsare non-negligible—an issue referred to as
the “black-soil problem”. Soil enhances both Rnir and
σF,distorting their intrinsic relationship. In this study,
we show that soil effects manifest through two
mainmechanisms: (1) direct soil reflection, which
significantly increases Rnir but has minimal impact on σF,
and (2)soil–vegetation multiple scattering, which affects
both Rnir and σF but tends to have compensatory
effects.Consequently, the dominant source of bias in the
original R2F relationship is direct soil reflection that
contributesto Rnir—a mechanism that had not been
explicitly isolated in previous studies. This finding allows
us tonarrow down the “black-soil problem” in the R2F
framework to the specific impact of soil single scattering
onRnir. To mitigate this bias, we propose a soil-adjusted
R2F (saR2F) method, which estimates the direct
soilcontribution of Rnir using TOC red and blue reflectance.
Correcting Rnir for the direct soil reflection results in
arobust relationship between σF and soil-adjusted Rnir
(saRnir), notably σF = saRnir/i0.We evaluated the saR2F
relationship using one field and two simulated datasets. In
the field study, saR2Fimproved the estimation of σF from
TOC reflectance, with R2 increasing ranging from 0.21 to
0.31 compared to the original R2F. In the two simulations,
saR2F consistently outperformed the original R2F, especially
under sparse canopy conditions. We also compared saR2F with
NDVI-based (NIRv) and FCVI-based R2F approaches. In the
available field observations collected under specific
conditions (i.e., varying viewing azimuth angles), the three
approaches showed similar performance and were better than
the original R2F in explaining the viewing- angle dependence
of σF. However, across the broader range of simulated
scenarios and for estimating the exact σF, saR2F
demonstrated better stability than NIRv and FCVI-based R2F
methods. The NIRv-based and FCVI-based R2F methods yielded
relatively low RMSE (0.092 and 0.075, respectively) but weak
explanatory power, with R2 values below 0.41 for canopies
with LAI <3. In contrast, saR2F achieved a much stronger
relationship (R2 =0.80) and a low RMSE of 0.044.
Furthermore, compared to the NIRv or FCVI-based approaches
for R2F corrections, saR2F offers a more physically
plausible and interpretable solution that can be applied to
angular correction and total SIF estimation. The effective
mitigation of the black-soil problem facilitates
interpretation of raw SIF observations and enhances the
monitoring of photosynthetic activity using SIF.},
cin = {IBG-2},
ddc = {550},
cid = {I:(DE-Juel1)IBG-2-20101118},
pnm = {1121 - Digitalization and Systems Technology for
Flexibility Solutions (POF4-112) / 2171 - Biological and
environmental resources for sustainable use (POF4-217)},
pid = {G:(DE-HGF)POF4-1121 / G:(DE-HGF)POF4-2171},
typ = {PUB:(DE-HGF)16},
UT = {WOS:001566835400001},
doi = {10.1016/j.rse.2025.114998},
url = {https://juser.fz-juelich.de/record/1045821},
}