Huey Creek is a meltwater stream that flows into the north end of Lake Fryxell in Taylor Valley. We conducted a comparative study to determine flow balances, flow routing in Huey Creek in 2006. The hypothesis is that truncated hydrographs on Huey Creek (and other streams) are related to large subsurface storage potential that fills/empties over the daily flood pulse. The goal of the simulation and experimental data comparison described here is to use a coupled groundwater / surface flow model to test this hypothesis.
Date Range:
2006-01-09
Data sources:
DOI:
10.6073/pasta/33da95cff96839639b202ea56d706467
Dataset ID:
8003