Aggregation in environmental systems – Part 2: Catchment mean transit times and young water fractions under hydrologic nonstationarity
Methods for estimating mean transit times from chemical or isotopic tracers (such as Cl<sup>−</sup>, <i>δ</i><sup>18</sup>O, or <i>δ</i><sup>2</sup>H) commonly assume that catchments are stationary (i.e., time-invariant) and homogeneous....
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2016-01-01
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| Series: | Hydrology and Earth System Sciences |
| Online Access: | http://www.hydrol-earth-syst-sci.net/20/299/2016/hess-20-299-2016.pdf |