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We found equal variance and no significant difference in mean stream discharge between hemlock- and hardwood-dominated streams.
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The results indicate that there were two primary spatial driving forces of wetland change in Peru's Cordillera Blanca from 1987 to 1995: 1) loss in glacier area was associated with increased wetland area, controlling for other factors; while 2) an increase in mean annual stream discharge in the previous 12 months increased wetland area.
Linear aspects include stream number, stream order, stream length, mean stream length, stream length ratio and bifurcation ratio.
Although neither stream discharge nor stream stage have been measured in the extension stream since its construction, it was observed that discharge and stream stage are comparable to or greater than discharge in the former upper Marx Creek.
Ultimately, calibration to hydraulic head and stream discharge occurred simultaneously, so the simulation that achieved final calibration to hydraulic head also achieved final calibration to stream discharge.
The model reproduced observed stream discharge patterns of the 14 sub-catchments and the dynamics of the 15 groundwater wells with an average accumulated discharge error of 1%15%5% standard deviation) and an average groundwater-level mean error of 0.1 m (0.23 m standard deviation).
During the wet period, the stream discharge increases transporting most of the stream sediments within the catchment.
Quantitative measurements of stream discharge, stream stage, and water depth in the extension stream have not yet been collected (W. Young personal communication 28 May 2013).
The model was manually calibrated to upper Marx Creek stream discharge and site groundwater levels.
Stream discharge measurements were recorded at weirs 1 15 of upper Marx Creek on 2 July 2007.
Stream discharge measurements were also used to calibrate the Marx Creek model.
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