Hello everyone,
I ran a WRF-Hydro simulation for one month at 4 km resolution using the CONUS404 dataset. The model ran smoothly; however, during my analysis of streamflow, I observed a high peak at the beginning of the simulation followed by an exponential decrease over time.
I am trying to understand whether this behavior is due to insufficient model spin-up or if it is related to an issue with the precipitation forcing data. In the CONUS404 dataset, precipitation is provided as accumulated grid-scale precipitation over the previous 60 minutes, which I converted to mm/s by dividing by 3600.
I have attached the streamflow plots for the simulated period for reference. I would greatly appreciate any guidance on whether this pattern indicates a spin-up issue or a potential problem with the forcing or model setup.
Thank you for your help.
Sherly
Dear Aubrey,
Thank you for your response.
I performed a one-year spin-up simulation from January 2018 to December 2018 and then ran the simulation for the year 2019. For the restart run, I used HYDRO_RST.2018-12-01_00:00_DOMAIN1 in hydro.namelist and RESTART.2018122700_DOMAIN1 in namelist.hrldas.
In addition, I enabled the following restart options:
I have attached the namelist files for your review. Please let me know if you notice any issues with the restart configuration.
Thank you for your time and assistance.
Best regards,
Sherly