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Low level moisture is important for triggering convection yet may be imprecisely predicted by the models.  Users should review the moisture content within the low-level inflow to areas with potential for significant convective development.  This can be done by comparing forecast values with available observations upstream (e.g. by comparing upstream dew points or vertical profiles).  Users should review the location of convective release and consider whether there is a possibility of deeper, more active convection.  See also examples of convection problems.

Forecast charts:

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