A double zero-inflated spatio-temporal model distinguishes true zeros from detection-limited zeros in precipitation using probit, Gamma, and Gaussian process components.
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The deep SPAR model shows concurrent floods and droughts becoming more likely in the Upper Danube by 2100 under high emissions, with changes in the dependence between catchments contributing substantially to the increase.
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Double zero-inflated spatio-temporal modeling of daily precipitation under detection thresholds
A double zero-inflated spatio-temporal model distinguishes true zeros from detection-limited zeros in precipitation using probit, Gamma, and Gaussian process components.