Hi there!
I understand that the ground heat flux, G, is the net heat flux from the atmosphere into the top of the ground. I am interested in the ground heat flux the way this term is used by glaciologists. They mean this ground flux to be the heat flux (also sometimes called subsurface/conductive heat flux) into the deeper ice levels after taking into account the heat loss to melting. This is normally calculated by a vertical temperature diffusion equation of the subsurface layers. Is this glaciological ground heat flux saved as an output variable or can it be calculated as a residual of variables outputted by the model (CESM1).
Specifically, I wonder if this ground flux is the FGR - FSM (where FSM is the snow melt heat flux). In that case, is a diffusion equation used to calculate FSM? In addition, what happens if the ice is directly exposed with no snow layer (only ice)?
Thank you in advance for any tips/hints!
Best,
Kirstin
I understand that the ground heat flux, G, is the net heat flux from the atmosphere into the top of the ground. I am interested in the ground heat flux the way this term is used by glaciologists. They mean this ground flux to be the heat flux (also sometimes called subsurface/conductive heat flux) into the deeper ice levels after taking into account the heat loss to melting. This is normally calculated by a vertical temperature diffusion equation of the subsurface layers. Is this glaciological ground heat flux saved as an output variable or can it be calculated as a residual of variables outputted by the model (CESM1).
Specifically, I wonder if this ground flux is the FGR - FSM (where FSM is the snow melt heat flux). In that case, is a diffusion equation used to calculate FSM? In addition, what happens if the ice is directly exposed with no snow layer (only ice)?
Thank you in advance for any tips/hints!
Best,
Kirstin