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Bed deformation models need to use the load (ice thickness) averaged over the duration of a time step of a bed deformation component.
A computationally expensive workaround: use synchronous coupling between mass continuity and bed deformation, i.e. bed deformation models take time steps as short as the rest of PISM.
Additional context
Whenever PISM takes short (in this context: shorter than a year) time steps and the climatic forcing resolves the annual cycle the modeled evolution of the ice thickness may contain a "high frequency" signal due to the SMB. For example: near a "steady state" the ice thickness would reach maximum in late winter and minimum in late summer, then increase towards the maximum over next winter and so on. This signal is especially noticeable when the system is near a "steady state" since it is not masked by a long term trend.
The current code (which uses instantaneous snapshots of ice thickness at the end of the current time step) suffers from aliasing of this high frequency signal. This can lead to all kinds of strange behavior, e.g.:
assuming constant year long time steps starting on January 1 and ending on December 31 (northern hemisphere): PISM's bed deformation code will use ice thickness near the maximum of the annual cycle for each time step
assuming constant year long time steps starting on October 1 and ending on September 30 (northern hemisphere): PISM's bed deformation code will use ice thickness near the minimum of the annual cycle for each time step.
The difference between corresponding loads may be small, but its influence can add up over time.
In most simulations time step lengths are chosen adaptively according to (CFL-based and SIA-diffusivity-based) stability criteria. This implies that any parameter change affecting ice speed, reporting frequency, etc may have an unpredictable and hard to understand influence on bed deformation.
The text was updated successfully, but these errors were encountered:
Why not have an accumulating-load variable, updated at each short time step, to approximate the time-integral of the load, which is then divided by the long time step to get the average load (and zeroed-out) at each bed deformation computation?
Description
Bed deformation models need to use the load (ice thickness) averaged over the duration of a time step of a bed deformation component.
A computationally expensive workaround: use synchronous coupling between mass continuity and bed deformation, i.e. bed deformation models take time steps as short as the rest of PISM.
Additional context
Whenever PISM takes short (in this context: shorter than a year) time steps and the climatic forcing resolves the annual cycle the modeled evolution of the ice thickness may contain a "high frequency" signal due to the SMB. For example: near a "steady state" the ice thickness would reach maximum in late winter and minimum in late summer, then increase towards the maximum over next winter and so on. This signal is especially noticeable when the system is near a "steady state" since it is not masked by a long term trend.
The current code (which uses instantaneous snapshots of ice thickness at the end of the current time step) suffers from aliasing of this high frequency signal. This can lead to all kinds of strange behavior, e.g.:
The difference between corresponding loads may be small, but its influence can add up over time.
In most simulations time step lengths are chosen adaptively according to (CFL-based and SIA-diffusivity-based) stability criteria. This implies that any parameter change affecting ice speed, reporting frequency, etc may have an unpredictable and hard to understand influence on bed deformation.
The text was updated successfully, but these errors were encountered: