Hi,
I want to simulate the mountain glacier evolution over Tibet Plateau using CESM2. So I have made a CISM grid with resolution of 1*1 km ( over the whole Plateau ) and altered the namelist (cism.config) correspondingly. According to the user guide at website "A.1 Introducing a new ice sheet grid — CESM Land Ice CESM2.0 documentation", I have also changed the GLACIER_REGION in CLM surface data and created the files "aave" and "blin" used by the coupler. With the above settings, the model can run with the compset "I1850Clm50SpG". However, the surface mass balance (smb) calculated by CLM always equals to 0 over the entire Tibet Plateau. Does anyone know the reason? ( I have modified the atmospheric forcing data to ensure the temperature is always below freezing point )
Thank you.
I want to simulate the mountain glacier evolution over Tibet Plateau using CESM2. So I have made a CISM grid with resolution of 1*1 km ( over the whole Plateau ) and altered the namelist (cism.config) correspondingly. According to the user guide at website "A.1 Introducing a new ice sheet grid — CESM Land Ice CESM2.0 documentation", I have also changed the GLACIER_REGION in CLM surface data and created the files "aave" and "blin" used by the coupler. With the above settings, the model can run with the compset "I1850Clm50SpG". However, the surface mass balance (smb) calculated by CLM always equals to 0 over the entire Tibet Plateau. Does anyone know the reason? ( I have modified the atmospheric forcing data to ensure the temperature is always below freezing point )
Thank you.