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Joint International Conference on Long-term Experiments ...

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%<br />

floods<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

0<br />

14<br />

12<br />

10<br />

I II III IV V VI VII VIII IX X XI XII<br />

m<strong>on</strong>ths<br />

Capusu Mare<br />

Aghires<br />

Mera(Radaia)<br />

Figure 4. M<strong>on</strong>thly floods frequency in Cluj- Dej Hills (1976-2004)<br />

8<br />

6<br />

4<br />

2<br />

0<br />

I II III IV V VI VII VIII IX X XI XII<br />

m<strong>on</strong>ths<br />

Borsa<br />

Luna de Jos<br />

Maia<br />

Figure 5. M<strong>on</strong>thly floods frequency in Cluj- Dej Hills (1976-2004)<br />

The m<strong>on</strong>thly frequency of floods formati<strong>on</strong> presents a maximum point in May, <strong>on</strong> the<br />

Almaş and Agrij rivers, in the Almaş-Agrij Depressi<strong>on</strong> (15 – 23% of the entire number<br />

of sorted floods), followed by March and June (with the same number of floods). The<br />

minimal frequency of floods or even their absence was recorded in November (Fig. 6)<br />

520

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