Hillslope-storage and rainfall-amount thresholds as controls of preferential stormflow
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Hillslope response to rainfall events was studied using 2D numerical experiments.

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Relationships between rainfall, stormflow, and leakage to bedrock were analyzed.

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Rainfall needed to initiate stormflow appeared as dynamic hillslope property.

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Hysteretic behavior of hillslope storage–discharge relationship obtained.

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Near-saturated conditions were sufficient to initiate significant stormflow.

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