Contrastingly, in downstream areas (Khaaraa3, Bayangol) river
discharge accumulates. Hence the gap between simulated water
availability and demand is almost closed, which is mirrored in low
calculated crop yield differences with and without water limitation.
Due to the absence of irrigated areas in the eastern sub-basins
(Bayan, Sugnugr, Kharaa 1, Tunkhelin), where runoff rates are high,
no increase in yield levels was observed
absence of