Dear all,
I used CLM5.0 in CESM2.1.2 for single point simulation, and the simulated site was FR Pue (Puechabon, France) (43.7413, 3.5957) The time is from 2000 to 2014, and the vegetation type is evergreen broad-leaved forest.
Atmospheric forcing data from half-hour observations at Fluxnet2015, surface data in 2000 were made by ./mknoocnmap.pl, mkmapdata.sh,./gen_domain and ./mksurfdata.pl utilities.
The compset I have chosen is I1PtClm50Bgc
(2000_DATM%1PT_CLM50%BGC_SICE_SOCN_SROF_SGLC_SWAV).
I used the entire data loop to run Spinup for 300 years, bringing the model to a stable state.
However, the variables of interest GPP and LH obtained differ significantly from actual observations, with LH being two to three times larger than the observed values. Here are the single point simulation results.
The attachment contains the Atmospheric driving and surface data, and log files.
Thank you for your feedback.


I used CLM5.0 in CESM2.1.2 for single point simulation, and the simulated site was FR Pue (Puechabon, France) (43.7413, 3.5957) The time is from 2000 to 2014, and the vegetation type is evergreen broad-leaved forest.
Atmospheric forcing data from half-hour observations at Fluxnet2015, surface data in 2000 were made by ./mknoocnmap.pl, mkmapdata.sh,./gen_domain and ./mksurfdata.pl utilities.
The compset I have chosen is I1PtClm50Bgc
(2000_DATM%1PT_CLM50%BGC_SICE_SOCN_SROF_SGLC_SWAV).
I used the entire data loop to run Spinup for 300 years, bringing the model to a stable state.
However, the variables of interest GPP and LH obtained differ significantly from actual observations, with LH being two to three times larger than the observed values. Here are the single point simulation results.
The attachment contains the Atmospheric driving and surface data, and log files.
Thank you for your feedback.

