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We could also separate the field into smaller batches and check whether any of these need
to be reconstructed.
There are ways to take this example further for those who wish. One could play around
with the amount of water that each cell shares. This will make it more expensive to calcu-
late but might give a smoother result. It's also possible to add pressure as a parameter,
making it possible for water to move up the slopes. Evaporation might be a way to remove
water from the system and clean up any puddles left by the main flow.
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