Aggregation in environmental systems – Part 2: Catchment mean transit times and young water fraction...
Aggregation in environmental systems – Part 2: Catchment mean transit times and young water fractions under hydrologic nonstationarity
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Copernicus Publications
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English
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Copernicus Publications
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Methods for estimating mean transit times from chemical or isotopic tracers (such as Cl−, δ18O, or δ2H) commonly assume that catchments are stationary (i.e., time-invariant) and homogeneous. Real catchments are neither. In a companion paper, I showed that catchment mean transit times estimated from seasonal tracer cycles are highly vulnerable to ag...
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Aggregation in environmental systems – Part 2: Catchment mean transit times and young water fractions under hydrologic nonstationarity
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TN_cdi_doaj_primary_oai_doaj_org_article_9d4d0f20d3074734bd6f389c3373ba4c
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_9d4d0f20d3074734bd6f389c3373ba4c
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ISSN
1607-7938,1027-5606
E-ISSN
1607-7938
DOI
10.5194/hess-20-299-2016
