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One way to deal with problems in very long time series (e.g. GlacierMIP) is to prevent grid points along the flowline to increase their area above a certain threshold (e.g. twice their original area), or at least for the mass-balance input.
This is very dirty though and I would prefer to avoid that.
The text was updated successfully, but these errors were encountered:
Related to that: 'RGI60-05.10315' (largest glacier in RGI05 with 23% of total RGI area) creates no runaway effect but reacts only very slowly, i.e., under stable climate conditions, it stabilises only after 1000-5000 years)
One way to deal with problems in very long time series (e.g. GlacierMIP) is to prevent grid points along the flowline to increase their area above a certain threshold (e.g. twice their original area), or at least for the mass-balance input.
This is very dirty though and I would prefer to avoid that.
The text was updated successfully, but these errors were encountered: