Dear WRF-Hydro users,
I am running offline WRF-Hydro v5.3 with reach-based routing for the Lake Tana, Upper Blue Nile Basin.
At the outlet of Lake Tana, the simulated wet-season peak occurs about 45 days earlier than observed and is substantially overestimated. The attached figure compares the observed discharge with the control run and several sensitivity experiments from January 1, 2006, to May 31, 2007.
Among the experiments, the three most recent were:
TEST08: Spatial soil and groundwater parameters improved the tributary simulations and slightly improved the lake outlet.
TEST09: Changes to LAKEPARM.nc produced CHANOBS results identical to TEST08.
TEST10: Large changes to routing parameters in Route_Link.nc, intended to delay the outlet flow, also produced results identical to TEST08.
I confirmed that selected CHANOBS_DOMAIN files from TEST08, TEST09, and TEST10 were byte-for-byte identical.
Could you please clarify:
Any guidance would be greatly appreciated.
Best regards,
Negusu

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Hi Arezoo,
Thank you for your quick and timely response.
I have attached the requested files: the namelists, Route_Link.nc, and LAKEPARM.nc.
I would greatly appreciate your guidance after you check the activated options and file settings.
Best
regards,
Negusu
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Hi Arezoo,
Thank you very much for testing the domain and identifying the issue. This is extremely helpful.
I will upgrade WRF-Hydro to version 5.4, keep the domain files and namelists unchanged, and correct the lake area to km².
Thank you also for checking the source code and confirming that the lake area should be provided in square kilometres. I will share the results after completing the new test and let you know if any issues remain.
Best regards,
Negusu