Laserfiche WebLink
<br />384 <br /> 0.90 <br /> 0.80 <br />. 0.70 <br />, <br /><; <br />> <br />c 0.60 <br />,9 <br />.~ 0.50 <br />u , <br /> .' <br /> 0.40 , <br /> 0,30 <br /> 0 <br />(,) <br /> 08 <br /> 0,6 <br />. <br />, <br />~ <br />c 04 <br />,9 <br />.~ <br />U <br /> 0,2 --':':~ <br /> 0,0 <br /> 0 <br />(b) <br /> <br />, <br /> <br />P.J. BR~MAUD AND Y.B. POINTIN <br /> <br />FORECASTING HEAVY RAINFALL FROM R.AIN CELL MOTION <br /> <br />385 <br /> <br />dHS5- 88 <br /> <br />CC 88 <br /> <br />o <br /> <br />,~..-- <br /> <br />'2 <br />"- -2 <br />E , <br />.s ---' <br />. ~ ,,- - <br />, -4 <br /><; <br />> <br />c <br />0 <br />, <br />-" -6 <br />"5 <br /> <br /> <br />--,-- <br /> <br /> <br />20 <br />STEP NUMBER <br /> <br />40 <br /> <br />20 <br />STEP NUMBER <br /> <br />40 <br /> <br />RI5 B8 <br /> <br />(e) <br /> 8 <br /> , <br />'2 , <br />"- 8 , <br />E , <br />.s <br />. <br />, 4 <br /><; <br />> <br />c <br />.g <br />-" 2 <br />" <br />u <br /> <br /> <br />dHS5;- 88 <br /> <br /> <br />20 <br />STEP NUMBER <br /> <br />40 <br /> <br />o <br />o <br /> <br />40 <br /> <br />20 <br />STEP NUMBER <br /> <br />(d) <br /> <br />Fig. 6. Efficiency curves of the methods PERS (dotted line), EXTRA (dashed line) and PARAPLUIE <br />(solid line) according to tbecritcria (a) ce. (b) RIS, (e) dHSS_ and (d)dHSS+ fOf the Cevennes 1988 event. <br /> <br />Fig. 6 (continued). <br /> <br />others (the SCOUT 11,0 method requires pictures without ground echoes), As <br />for Figs, 6(a)-6(d), the PERS, EXTRA, SCOUT 11,0 and PARAPLUIE <br />methods are depicted with dotted line, dashed line, dash-dotted line and solid <br />line, respectively, The Paris 1989 event is characterized by the development of <br />isolated stonns, and the interval between radar pictures is 5 min. <br />The results of Figs, 7(a)-7(d) show that the PERS method gives a signifi- <br />cantly poorer performance during the Paris 1989 event than during the <br />Cevennes 1988 one, This is due to the smaller number of rainy pixels in this <br />event for which an efficient rainfall forecast is really needed, As for the results <br />of Figs, 6(a)-6(d), the PARAPLUIE method tends to forecast the rain better <br /> <br />than the other methods, but the differences between the PARAPLUIE and the <br />EXTRA methods are smaller for the Paris 1989 event because the motions of <br />the radar echoes are much more homogeneous during that event than during <br />the Cevennes 1988 one, <br />According to the efficiency curves of the CC, RI and, in particular, the dHS <br />criteria, shown in Figs, 7(a), 7(b) and 7(d) respectively, the SCOUT II,O result; <br />are characterized by slightly worse performances than that of PARAPLUIE, <br />Moreover, the SCOUT II,O method tends to underestimate the observed rain <br />more than the PARAPLUIE method does (Fig, 7(c)), During this event, the <br />EXTRA method detects the global motion of all the isolated stonns, the <br /> <br />