Exact(2)
In both catchments, we monitored overland flow from hillslope plots and stream runoff from catchments at basin outlets over a 2-year pre-thinning period and a 2-year post-thinning period.
Concentrations and loads of P in quickflow (QF) were measured at basin outlets during four storm events and were compared with dynamic (QF magnitude) and static (extent of highly-connected, poorly-drained soils) transport metrics and a CSA metric (extent of highly-connected, poorly-drained soils with excess plant-available P).
Similar(58)
Simulated discharges from the gauged and reanalysis rainfall data, respectively, are analysed and compared with the observed discharge in basin outlet over the period 1991 2005.
The model correctly reproduces the observed discharge at the basin outlet.
In both cases, the variational DA (VAR) technique was used to assimilate discharge data at the basin outlet.
Finally, we explore the value of using discharge observations at interior points in model calibration by assessing gains/losses in hydrograph simulations at the basin outlet.
The discharge at the basin outlet has declined at a rate of 3388 × 106 m3 decade−1, suggesting the need of environmental flow assessment.
In concrete terms, 68 measurements of stream discharge and bed load transport rate were carried out at a location, near the basin outlet.
The direction and timing of vegetation change differed with landscape position along a gentle elevation gradient from the basin outlet to a nearby volcanic ridge top.
C4 perennial grasses have dominated the basin outlet, center, and toe slope landscape positions since at least 5000 6000 years BP, except for the dominance of C3 plants at the bottom of the outlet excavation at 5000 years BP.
The highest point of this basin is Soltan Sanjar Mt with 3200 meter elevation in the east and the lowest point is on the basin outlet in boundary city of Jolfa 300m elevation.
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