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Fricker et al 25 confirmed and generalised these results As an example, the average footprint area in which an F5 tornado reaches F5 intensity is only about 2% of its total footprint area We use these results and Equation (1) to estimate the local hit rate with given intensity The result are tornado risk climatologies for the US by intensity These risk climatologies can be combined. Click here👆to get an answer to your question ️ If xi 's are the mid points of the class intervals of grouped data, f1 's are the corresponding frequencies and x̅ is the mean, then ∑ (fi xi x̅) is equal to. $ o , ÷ 262qC o p/v*D60% o p5 ö30% v ÷Ta=25 qC â G Þ Ð Ö Ú ã È é M ù 4Ú ¸Ob ê ¿ Ê æ å Æ9ë % (1) , 6 4 f # 3 o < â ½ Æ Table 2 Ob= (2) P=500W â50%/v*D $ o , ÷ 255qC Tj=Tc TJCP =62qC10qC / Wu030W=65qC Ò Ú Ç Þ áTable 4 ST=34 (3) Table 5 SS=0054 (4) Table 6 SC= (5) Table 7 SQ=24 (6) Table 8 SE=90 (7) Op=ObuSTuSSuSCuSQuSE/10 6 (4F = /106 (4F.

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Fuzzy DEA models 25, to formulate the fuzzy network DEA When the input and output data are all crisp numbers, the fuzzy network DEA boils down to a conventional one Third, to reduce the flexibility of weights and improve the discrimination of the DEA model, this study imposes weight restrictions on the proposed model This paper is organized as follows In the next section, a. "Þ6õ gcg2ghh >â>Ú>á>Ì?$>Ì>Þ>Ú>Þ>Ìh gÛh h >úg >ô>ûh È gg 2Ã ) h >úh gcg2ghh >â>Ú>á>Ì?$>Ì>Þ>Ú>Þ>Ì>ÔgÛ>Õ h >ô>ûh gcg2ghh >á>Ú>â>Ì.