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@ARTICLE{Guan:1048831,
author = {Guan, Buliao and Naz, Bibi and Hendricks-Franssen,
Harrie-Jan and Vereecken, Harry},
title = {{I}dentifying uncertainties in snowpack variables using
ensemble-based simulations of {CLM}5 over {A}lpine {S}ites},
journal = {Journal of hydrology},
issn = {0022-1694},
address = {Amsterdam [u.a.]},
publisher = {Elsevier},
reportid = {FZJ-2025-04939},
year = {2025},
abstract = {Snow plays a pivotal role in the hydrological cycle,
influencing surface energy and water balances in the
snow-dominated regions. Land surface models such as CLM5
(Community Land Model version 5) offer a valuable tool to
study snow processes and their impact on water resources,
but identifying sources of uncertainties is important as
meteorological forcings and parameters errors limit the
accuracy of snow-related land surface model prediction. To
identify sources of uncertainties in snow simulation, we
conducted ensemble-based simulations of CLM5 across 10 sites
in the French Alps for the period 1991-2022 using
meteorological inputs from bias corrected ECMWF Reanalysis
v5 (ERA5). Three ensemble experiments were performed to
isolate different sources of uncertainty by perturbing (1)
only snow-related parameters, (2) only atmospheric forcings,
and (3) both combined. Model performance was evaluated at
each site using 100 ensemble members against in-situ snow
depth (SD) and remotely sensed snow cover fraction (SCF)
observations using statistical metrics such as correlation
(R), Root Mean Square Error (RMSE) and ensemble spread skill
(SS). Our results show that observations are better captured
in the combined experiment, with forcing uncertainties
having a greater impact on model performance than parameter
uncertainties as reflected by relatively higher ensemble SS
values in both forcings and combined experiments (SD mean
SS: 0.133 for parameters, 0.222 for forcing, 0.292
combined). However, the low SS values indicate that the
ensemble spread does not fully capture the ensemble mean
error across all three experiments. Furthermore, the model
captures 30 observational variability more effectively
during the accumulation season than during the ablation
season, as reflected by higher SS values and lower RMSE in
the combined experiment (Snow depth ablation: mean SS:
0.299, and mean RMSE: 0.229m. Accumulation SS: 0.285, and
RMSE: 0.357m). In addition, CLM5 shows the lowest ensemble
skill for both snow depth (SD) and snow cover fraction (SCF)
for sites at high-elevation sites (>1800 m), while grassland
sites show better agreement with observations than forested
sites, likely due to the reduced complexity of snowpack
processes in the absence of canopy–snow interactions.
These findings are useful for improving uncertainty
characterization, reducing model errors, and support the
development of snowpack data assimilation in land surface
modeling.},
cin = {IBG-3},
ddc = {690},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2152 - Water resources and the environment (POF4-215) /
2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217) / SFB 1502 C04 - Assimilation von
Schnee-Satellitendaten und ihre Auswirkungen auf den
hydrologischen Kreislauf und die atmosphärischen Flüsse
(C04) (495864060)},
pid = {G:(DE-HGF)POF4-2152 / G:(DE-HGF)POF4-2173 /
G:(GEPRIS)495864060},
typ = {PUB:(DE-HGF)25},
url = {https://juser.fz-juelich.de/record/1048831},
}