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References (23)
-
J. McDonnell (1988)
The age, origin and pathway of subsurface stormflow in a steep humid headwater catchment. -
J. Gat, W. Dansgaard (1972)
Stable isotope survey of the fresh water occurrences in Israel and the Northern Jordan Rift ValleyJournal of Hydrology, 16
-
S. Matsuo, I. Friedman (1967)
Deuterium content in fractionally collected rainwaterJournal of Geophysical Research, 72
-
P. Hartley (1981)
Deuterium/hydrogen ratios in Australian rainfallJournal of Hydrology, 50
-
J. Heathcote, J. Lloyd (1986)
Factors affecting the isotopic composition of daily rainfall at Driby, LincolnshireInternational Journal of Climatology, 6
-
H. Craig (1961)
Standard for Reporting Concentrations of Deuterium and Oxygen-18 in Natural WatersScience, 133
-
Bonell (1981)
Soil hydraulic properties and their effect on surface and subsurface water transfer in a tropical rainforest catchmentHydrol. Sci. J.
-
D. Ehhalt, K. Knott, J. Nagel, J. Vogel (1963)
Deuterium and oxygen 18 in rain waterJournal of Geophysical Research, 68
-
Jackson Jackson (1987)
Hydrology of an acid wetland before and after draining for afforestation, western New Zealand, Proceedings of the Vancouver Symposium, August 1987IAHS Publ.
-
J. Turner, D. Macpherson, R. Stokes (1987)
The mechanisms of catchment flow processes using natural variations in deuterium and oxygen-18Journal of Hydrology, 94
-
A. Pearce, M. Stewart, M. Sklash (1986)
Storm runoff generation in humid headwater catchments 1 -
Pearce Pearce, Rowe Rowe, O'Loughlin O'Loughlin (1984)
Hydrology of mid‐altitude tussock grasslands, Upper Waipori catchment, II, Water balance, flow duration and storm runoffJ. Hydrol. NZ
-
D. Bottomley, D. Craig, L. Johnston (1984)
Neutralization of acid runoff by groundwater discharge to streams in Canadian Precambrian Shield watershedsJournal of Hydrology, 75
-
V. Kennedy, Gray Zellweger, R. Avanzino (1979)
Variation of rain chemistry during storms at two sites in northern CaliforniaWater Resources Research, 15
-
V. Kennedy, C. Kendall, G. Zellweger, T. Wyerman, R. Avanzino (1986)
Determination of the components of stormflow using water chemistry and environmental isotopes, Mattole River basin, CaliforniaJournal of Hydrology, 84
-
M. Sklash, M. Stewart, A. Pearce (1986)
Storm Runoff generation in humid headwater catchments 2. A case study of hillslope and low-order stream responseWater Resources Research, 22
-
W. Dansgaard (1964)
Stable isotopes in precipitationTellus A, 16
-
M. Sklash, R. Farvolden, P. Fritz (1976)
A conceptual model of watershed response to rainfall, developed through the use of oxygen-18 as a natural tracerCanadian Journal of Earth Sciences, 13
-
Pearce Pearce, Stewart Stewart, Sklash Sklash (1986)
Storm runoff generation in humid headwater catchments, 1, Where does the water come from?Water Resour. Res.
-
M. Stewart (1975)
Stable isotope fractionation due to evaporation and isotopic exchange of falling waterdrops: Applications to atmospheric processes and evaporation of lakesJournal of Geophysical Research, 80
-
A. Pearce, L. Rowe, C. O'louglin (1984)
Hydrology of mid-altitude tussock grasslands, upper Waipori catchment. II: Water balance, flow duration and storm runoffJournal of hydrology. New Zealand, 23
-
M. Sklash, R. Farvolden (1979)
The Role Of Groundwater In Storm RunoffJournal of Hydrology, 43
-
M. Bonell, A. Pearce, M. Stewart (1990)
The identification of runoff‐production mechanisms using environmental isotopes in a tussock grassland catchment, eastern otago, New ZealandHydrological Processes, 4
- Publisher
- Wiley
- Copyright
- Copyright © 1990 by the American Geophysical Union.
- ISSN
- 0043-1397
- eISSN
- 1944-7973
- DOI
- 10.1029/WR026i003p00455
- Publisher site
- See Article on Publisher Site
Abstract
Isotopic variation in storm rainfall is an important consideration in hydrograph separation using the mass balance approach but is rarely considered when determining the accuracy of old water estimates. Study of a small watershed on the South Island of New Zealand in which new water is a major component of the storm hydrograph shows that, in addition to the within‐storm isotopic variations themselves, rainfall weighting techniques may substantially influence estimates of old/new water as a function of both total runoff and total quick flow production. Two incremental approaches to rainfall weighting are presented. Results show that within‐storm incremental weighting is better than the standard weighting technique, which imposes a total storm rainfall value exogenously on the mass balance equation.
Journal
Water Resources Research – Wiley
Published: Mar 1, 1990