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WATER & SOIL - These are not the droids you are looking for.

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F.3 Analysis and results<br />

tatively placed with<br />

Region on <strong>the</strong> basis<br />

<strong>the</strong> hydrograph <strong>for</strong><br />

to <strong>the</strong> Taieri River<br />

Paerau and Loganburn at Paerau (Figure F. l0)<br />

Southland rivers (Figure F.9).<br />

-<br />

than <strong>the</strong><br />

(see section 3.1.6). Plots with similar shape were overlaid to<br />

<strong>for</strong>m combined plots.<br />

Flood frequency data thus plotted were found to lie in<br />

three groups:<br />

(a) peak lake inflows and Shotover floods;<br />

(b) Southland floods and <strong>the</strong> pomahaka floods;<br />

(c) East Otago floods.<br />

Group (a) closely resembled <strong>the</strong> South Island West Coast<br />

data<br />

Canterbury data<br />

(see<br />

<strong>the</strong>se two groups<br />

were<br />

I plots of <strong>the</strong> data<br />

<strong>the</strong>y<br />

Support <strong>for</strong> <strong>the</strong> differentiation of <strong>the</strong> lake inflows and<br />

Shotover from <strong>the</strong> o<strong>the</strong>r sites studied is also given by <strong>the</strong><br />

hydrographs (Figure F.8). <strong>These</strong> show that floods <strong>are</strong> frequent<br />

and occur at <strong>the</strong> same time <strong>for</strong> each catchment. Since<br />

<strong>the</strong> floods result from <strong>the</strong> same storms, it is an argument<br />

<strong>for</strong> each catchment having a similar shape in its flo;d frequency<br />

curve and <strong>for</strong> grouping <strong>the</strong>m toge<strong>the</strong>r. Also shown<br />

in Figure F.8 is <strong>the</strong> hydrograph <strong>for</strong> Cieddau at Mil<strong>for</strong>d.<br />

Finally,<br />

-<br />

<strong>the</strong> hydrographs (Figures F.8, F.9 F.lO) show<br />

that <strong>the</strong> majority of large floods in <strong>the</strong> decade l97l-19g0<br />

o-ccurred in <strong>the</strong> years 1978-1980. Figures <strong>for</strong> F.g, F.9, F.l0<br />

also show <strong>the</strong> wide extent of <strong>the</strong> October l97g flood which<br />

was <strong>the</strong> largest of <strong>the</strong> decade <strong>for</strong> many of <strong>the</strong> records.<br />

F.4 Gonclusion<br />

and <strong>the</strong> Manuherikia at Ophir (1971-1980) wirh rhe<br />

regional clrves (Figure F.7) shows <strong>the</strong> difficulty in determining<br />

which curve is appropriate. Central Otágo is ten_<br />

graphs (Figures F.8, F.9, F.l0)<br />

because <strong>the</strong> frequency of minor<br />

ach region but <strong>not</strong> across region<br />

ïable F.3 Co-ordinates fiom regional frequency curves.<br />

O2.33/O<br />

o5/o<br />

olo/o<br />

ozdo<br />

o5o/o<br />

orodo<br />

ozoo/o<br />

S.l. West<br />

Coast<br />

1.OO<br />

1.24<br />

1.45<br />

1.64<br />

1.89<br />

2.O8<br />

2.27<br />

Southland<br />

1.03<br />

1.46<br />

1.82<br />

2.16<br />

2.61<br />

2.94<br />

3.27<br />

sth<br />

Canterbury-<br />

Otago<br />

0.97<br />

1.51<br />

1.99<br />

2.48<br />

3.17<br />

3.73<br />

4.33<br />

Acknowledgements<br />

D. McMillan in compiling <strong>the</strong><br />

Miss K. Vollebregt in anatysing<br />

owledged.<br />

References<br />

Fitzharris, B.B.; Stewart, D; Harrison, W. l9g0: Contribution<br />

of snowmelt to <strong>the</strong> October l97g flood of <strong>the</strong><br />

Pomahaka and Fraser Rivers, Otago. Journal o!<br />

Hydrologlt (NZ) I9(2): 84-93.<br />

Gilbert, D.J. 1978: Calculating lake inflow. Journal o!<br />

Hydrologlt (NZ) I 7(I): 3943.<br />

Ministry of Works: Hydrology Annual. (No. 3, 1955 ...<br />

No. 17, 1969). Ministry of Works, Wellington.<br />

t2Á Water & soil technical publication no. 20 (1982)

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