Dear Icepack Consortium Team,
I am currently running the latest standalone version of Icepack (v1.5.3) using ERA5 atmospheric forcing data. I have attached my icepack_in configuration file, forcing file (ERADATA.txt), and the model run log for reference.
While analyzing the simulations, I noticed that the model-simulated surface temperature is consistently colder than the observed/forcing atmospheric temperature. I would like to clarify whether this behavior is physically acceptable in standalone Icepack simulations or whether it may indicate an issue in my setup or forcing configuration.
I am particularly concerned because this surface temperature bias could affect the surface energy balance, especially the sensible and latent heat flux calculations. Since these fluxes depend strongly on the temperature gradient between the surface and atmosphere, I suspect that the colder surface temperature may be enhancing sublimation and contributing to an underestimation of snow depth in my simulations.
In my runs, the model is not able to reproduce the observed snow depth evolution well, and sublimation appears relatively high. I am unsure whether this is:
Thank you very much for your time and guidance.
Best regards,
Ajay Bhadran
I am currently running the latest standalone version of Icepack (v1.5.3) using ERA5 atmospheric forcing data. I have attached my icepack_in configuration file, forcing file (ERADATA.txt), and the model run log for reference.
While analyzing the simulations, I noticed that the model-simulated surface temperature is consistently colder than the observed/forcing atmospheric temperature. I would like to clarify whether this behavior is physically acceptable in standalone Icepack simulations or whether it may indicate an issue in my setup or forcing configuration.
I am particularly concerned because this surface temperature bias could affect the surface energy balance, especially the sensible and latent heat flux calculations. Since these fluxes depend strongly on the temperature gradient between the surface and atmosphere, I suspect that the colder surface temperature may be enhancing sublimation and contributing to an underestimation of snow depth in my simulations.
In my runs, the model is not able to reproduce the observed snow depth evolution well, and sublimation appears relatively high. I am unsure whether this is:
- A normal limitation or expected behavior in standalone Icepack simulations,
- Related to uncertainties or biases in the atmospheric forcing,
- Associated with parameter choices in the thermodynamic scheme, or
- Indicative of a mistake in my setup or forcing preparation.
Thank you very much for your time and guidance.
Best regards,
Ajay Bhadran