Hita lafudhi la kitengo
Hita lafudhi la kitengo (UH) ni mabadiliko ya mstari ambayo hubadilisha mvua ya ziada kuwa mtiririko wa maji kwa bonde la mto. Imeanzishwa na Sherman mnamo 1932, UH inadhani kuwa mwitikio wa mvua-mtiririko ni wa mstari na haubadiliki kwa wakati, ikiruhusu usanisi wa hita lafudhi za mafuriko kutoka kwa dhoruba za muundo kwa ajili ya kubuni chemichemi za mabwawa na tathmini ya hatari ya mafuriko.
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Method map
The neighbourhood of related methods — select a node to explore.
Vyanzo
- Sherman, L. K. (1932). Streamflow from rainfall by the unit graph method. Engineering News-Record, 108(14), 501-505. link ↗
- Snyder, F. F. (1938). Synthetic unit-graphs. Transactions of the American Geophysical Union, 19(1), 447-454. DOI: 10.1029/TR019i001p00447 ↗
- Clark, C. O. (1945). Storage and the unit hydrograph. Journal of the American Water Works Association, 37(4), 419-432. link ↗
Jinsi ya kunukuu ukurasa huu
ScholarGate. (2026, June 3). Unit Hydrograph Theory for Rainfall-Runoff Transformation. ScholarGate. https://scholargate.app/sw/civil-engineering/unit-hydrograph
Which method?
Set this method beside its closest kin and read them side by side — the library lays the books on the table; the choice is yours.
- Uundaji wa Modeli ya Maji ya Chini ya Ardhi kwa kutumia MODFLOWUhandisi wa Ujenzi↔ compare
- Njia ya MuskingumUhandisi wa Ujenzi↔ compare
- Traffic Flow (LWR Model)Uhandisi wa Ujenzi↔ compare
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