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Sub-grid variability (notably for rainfall but other parameters too) can be addressed by downscaling.  Downscaling converts the

Downscaling converts:

•  the average grid box

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• probability density functions from

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• raw

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• ENS into
• "point rainfall probability density functions" for points within

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• the grid box.

New downscaling techniques are being developed accordingly (see for example the Point Rainfall product).

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