By Milan K. Jermar
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Extra info for Water Resources and Water Management
E . p r e c i p i t a t i o n from the upper p a r t of the atmosphere system, characterized by a v e r t i c a l movement of drops: d r i z z l e , r a i n , snow, g l a z e , h a i l , sleet e t c . , (b) h o r i z o n t a l , i . e . water eliminated by condensation o r sublimation on the ground: dew, hoar f r o s t , rime, diamond d u s t e t c . Depending on i t s s t a g e of agglomeration, p r e c i p i t a t i o n is e i t h e r l i q u i d o r s o l i d . I t is measured i n terms of depth (mn), r a i n f a l l i n t e n s i t y i n t e r n of 19 mn per minute.
000 1 500 -0,015 S sediment transport ; 2 - 100 P a r t i a l c o e f f i c i e n t f o r estimation of the roughness c o e f f i c i e n t f o r various boundaries according t o Cowan (1957) supplemented by t h e c o e f f i c i e n t of the sediment t r a n s p o r t impact. 4 INTERREIATIONS OF SLJRFACF WATER AND GROllNJWATER RLTNOFF Runoff is a hydrologic process of r a i n f a l l d i s t r i b u t i o n by the E a r t h ' s sinface, which takes place i n thc system of the l i t h o - and hydrosphere.
Four tanks arranged v e r t i c a l l y f o r humid a r e a s , s e v e r a l rows of four tanks arranged v e r t i c a l l y f o r semi-arid and a r i d Fig. 1 . 1 2 . Separation of the runoff components, its course and physical principles of the mtheniatical m d e l of t h e runoff process according t o SUGAWAHA (1974): ql - s u r f a c e r u n o f f , % ground s u r f a c e , 93 - intermediate outflow groundwater runoff with short-term and q (above the groundwater t a b l e ) , with long-term delay before p e n 3 r a t i o n i n t o t h e r i v e r , 21 infiltration, 22,23 - p e r c o l a t i o n i n t o groundwater, 24 deep p e r c o l a t i o n .
Water Resources and Water Management by Milan K. Jermar