Faculty mentor: Gabriel Bowen
The relative abundance of heavier H and O isotopes indicates what season water fell as precipitation. A Seasonal Origin Index quantifies whether winter or summer precipitation is more represented in streamflow and evapotranspiration. Calculating a Young Water Fraction measures the fraction of water in a catchment that is younger than about 2.3 months. End-Member Splitting Analysis tells what fraction of streamflow and evapotranspiration originated as winter or summer precipitation.
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