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Reply to comment on ‘Characterization of surface and ground water δ18O seasonal variation and its use for estimating groundwater residence times’ by R. E. Criss and W. E. Winston

✍ Scribed by Michael M. Reddy; Paul Schuster; Carol Kendall; Micaela B. Reddy

Publisher
John Wiley and Sons
Year
2006
Tongue
English
Weight
102 KB
Volume
20
Category
Article
ISSN
0885-6087

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Characterization of surface and ground w
Characterization of surface and ground water δ18O seasonal variation and its use for estimating groundwater residence times
✍ Michael M. Reddy; Paul Schuster; Carol Kendall; Micaela B. Reddy 📂 Article 📅 2006 🏛 John Wiley and Sons 🌐 English ⚖ 349 KB

18 O is an ideal tracer for characterizing hydrological processes because it can be reliably measured in several watershed hydrological compartments. Here, we present multiyear isotopic data, i.e. 18 O variations (υ 18 O), for precipitation inputs, surface water and groundwater in the Shingobee Riv

Comment on ‘M. M. Reddy, P. Schuster, C.
Comment on ‘M. M. Reddy, P. Schuster, C. Kendall and M. B. Reddy, characterization of surface and ground water δ18O seasonal variation and its use for estimating groundwater residence times. Hydrological Processes 20 (2006) this issue’
✍ R. E. Criss; W. E. Winston 📂 Article 📅 2006 🏛 John Wiley and Sons 🌐 English ⚖ 137 KB

## Abstract Reddy __et al__. (2006, __Hydrological Processes__ **20**: 1753–1772) disregard germane published data and successful isotopic models, selectively depict data from their data sets, misplot many of their data, and use poorly correlated sinusoidal fits to their data to derive erroneous hy