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Until the mid-20th century, the Red River contributed flow to both the Atchafalaya and, via the Old River, the Mississippi.
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We developed a runoff response model by simply determining the hydrologic connectivity from a DEM or DTM and adding the elementary responses of contributing flow paths at any point along a stream or drainage channel.
The results revealed that the SWAT model over-predicted the areas contributing flow for events with lower rainfall; while for the events with higher rainfall amount the model closely simulated the time-varying contributing area.
Multiple (three) porosity domains contributed to flow at the highest rainfall intensities, including preferential flow through macropore pathways.
JS, VP, AJ, and SG contributed to flow cytometry experiments.
EG contributed in flow cytometry and transfection experiments.
TH processed specimens and contributed to flow cytometry panel design.
Yi Wen Yang contributed to flow cytometry and confocal microscope observation.
WTH performed mouse studies and contributed to flow cytometry data acquisition and analysis, and performed RNA isolation.
According to this model, the cross-sectional area of the airway, the compliance of the airway, and the resistance upstream from the flow limiting segment all contribute to flow limitation.
Temporal dynamics inferred heterogeneous montane groundwater bodies contributed to flows differentially during the recession.
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