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Second, based on the results of the first step, the forecasted rainfall from each station is used to obtain the spatial characteristics of the rainfall process is presented.
Residents often struggle to differentiate between the probability of a forecasted event and forecast confidence.
The propagation of the data assimilation correction to gauging stations located upstream or downstream of the assimilated stations limited the deterioration of forecasted streamflow due to real-time conditions.
At stations MY, KM, and OF, the forecasted onsets of the first tsunamis roughly match the observations.
Results suggest that the algorithm leading to the best (highest) correlation coefficient between forecasted and monitored values is LR, with an r ranging from 0.406 for station AM3 up to 0.641 for station AM4 for the GMA.
5.3.1 Sales Forecast The following table and chart highlight forecasted sales.
The forecasted individual factors are combined to obtain the forecasted TEC values.
Four different seasons are forecasted and it is also possible to consult forecasts made previously.
At tide-gauge stations MY, KM, and OF on the northern Tohoku coast, the forecasted heights of the first tsunamis were greater than 10 m, while the actual heights already reached larger than 4 m at this time (Fig. 3(d)).
5.2.1 Sales Forecast The following table and chart give a run-down on forecasted sales.
The second map shows the forecasted temperatures for 2050.
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