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T. Osterkamp, M. Payne (1981)
Estimates of permafrost thickness from well logs in northern AlaskaCold Regions Science and Technology, 5
R. Linsley, M. Kohler, J. Paulhus (1958)
Hydrology for engineers
K. Eshleman, J. Pollard, A. O'brien (1993)
Determination of contributing areas for saturation overland flow from chemical hydrograph separationsWater Resources Research, 29
M. Hinton, S. Schiff, M. English (1994)
Examining the contributions of glacial till water to storm runoff using two‐ and three‐component hydrograph separationsWater Resources Research, 30
(1992)
Testing the groundwater idging hypothesis of streamflow generation during snowmelt
L. Hinzman, D. Kane, R. Gieck, K. Everett (1991)
Hydrologic and thermal properties of the active layer in the Alaskan ArcticCold Regions Science and Technology, 19
D. Kane, J. Stein (1983)
Water movement into seasonally frozen soilsWater Resources Research, 19
J. McDonnell, M. Stewart, I. Owens (1991)
Effect of Catchment‐Scale Subsurface Mixing on Stream Isotopic ResponseWater Resources Research, 27
C. Wels, Colin Taylor, R. Cornett, B. Lazerte (1991)
Streamflow generation in a headwater basin on the precambrian shieldHydrological Processes, 5
N. Roulet, M. Woo (1988)
Runoff generation in a low Arctic drainage basinJournal of Hydrology, 101
R. Hooper, C. Shoemaker (1986)
A Comparison of Chemical and Isotopic Hydrograph SeparationWater Resources Research, 22
Kreit Kreit, Peterson Peterson, Corliss Corliss (1992)
Water and sediment export of the upper Kuparuk River drainage of the North Slope of AlaskaHydrobiologica, 240
(1992)
Water and sediment export of the upper Kuparuk River drainage of the North Slope of Alaska , Hydrobiologica
(1972)
Late Cenezoic glaciation of the Central Brooks Range , in Glaciation in Alaska : The geologic record
S. Hastings, S. Luchessa, W. Oechel, J. Tenhunen (1989)
Standing biomass and production in water drainages of the foothills of the Philip Smith Mountains, AlaskaEcography, 12
T. Dinçer, B. Payne, T. Florkowski, J. Martinec, E. Tongiorgi (1970)
Snowmelt runoff from measurements of tritium and oxygen‐18Water Resources Research, 6
A. Rodhe (1981)
Spring Flood Meltwater or GroundwaterHydrology Research, 12
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
D. Kane, L. Hinzman, C. Benson, K. Everett (1989)
Hydrology of Imnavait Creek, an arctic watershedEcography, 12
L. Cooper, C. Olsen, D. Solomon, I. Larsen, R. Cook, J. Grebmeier (1991)
Stable Isotopes of Oxygen and Natural and Fallout Radionuclides Used for Tracing Runoff During Snowmelt in an Arctic WatershedWater Resources Research, 27
D. Pilgrim, D. Huff, T. Steele (1979)
Use of specific conductance and contact time relations for separating flow components in storm runoffWater Resources Research, 15
J. McNamara, D. Kane, L. Hinzman (1998)
An analysis of streamflow hydrology in the Kuparuk river basin, Arctic Alaska : A nested watershed approachJournal of Hydrology, 206
R. Freeze (1972)
Role of subsurface flow in generating surface runoff: 1. Base flow contributions to channel flowWater Resources Research, 8
(1993)
Comparison of snowmelt hydrograph separation by recession analysis and by stream temperature and conductance
(1986)
Determination of the components of storm flow using water chemistry and environmental isotopes
J. Buttle, K. Sami (1992)
Testing the groundwater ridging hypothesis of streamflow generation during snowmelt in a forested catchmentJournal of Hydrology, 135
(1997)
An analysis of streamflow hydrology in the Kuparuk River basin : A nested watershed approach
D. Peters, J. Buttle, Colin Taylor, B. Lazerte (1995)
Runoff Production in a Forested, Shallow Soil, Canadian Shield BasinWater Resources Research, 31
(1989)
Wetland soils and vegetation
G. Weller, F. Chapin, K. Everett, J. Hobbie, D. Kane, W. Oechel, C. Ping, W. Reeburgh, D. Walker, J. Walsh (1995)
The arctic flux study: A regional view of trace gas releaseJournal of Biogeography, 22
M. Walker, D. Walker, K. Everett, C. Segelquist (1989)
Wetland Soils and Vegetation, Arctic Foothills, Alaska.
(1981)
Spring flood - - Melt water or groundwater ?
D. Kane, L. Hinzman, C. Benson, G. Liston (1991)
Snow hydrology of a headwater Arctic basin: 1. Physical measurements and process studiesWater Resources Research, 27
D. Bottomley, D. Craig, L. Johnston (1986)
Oxygen-18 studies of snowmelt runoff in a small Precambrian shield watershed: Implications for streamwater acidification in acid-sensitive terrainJournal of Hydrology, 88
S. Dingman (1971)
HYDROLOGY OF THE GLENN CREEK WATERSHED, TANANA RIVER BASIN, CENTRAL ALASKA
T. Hamilton (1986)
Late Cenozoic Glaciation of the Central Brooks Range
L. Cooper, C. Solís, D. Kane, L. Hinzman (1993)
Application of Oxygen-18 Tracer Techniques to Arctic Hydrological ProcessesArctic and alpine research, 25
D. Dewalle, B. Swistock, W. Sharpe (1988)
Three-component tracer model for stormflow on a small Appalachian forested catchmentJournal of Hydrology, 104
Hillslope hydrology in an Arctic setting , paper presented at the Sixth International Conference on Permafrost
M. Woo, P. Steer (1983)
SLOPE HYDROLOGY AS INFLUENCED BY THAWING OF THE ACTIVE LAYER, RESOLUTE, N.W.T.Canadian Journal of Earth Sciences, 20
M. Sklash, R. Farvolden (1979)
The Role Of Groundwater In Storm RunoffJournal of Hydrology, 43
Storm hydrographs in the Upper Kuparuk River basin (142 km2) in northern Alaska were separated into source components using a mixing model and by recession analysis. In non‐Arctic regions, storm flow is commonly dominated by old water, that is, water that existed in the basin before the storm. We suspected that this may not be true in Arctic regions where permafrost diminishes subsurface storage capacity. Streamflow during the snowmelt period was nearly all new water. However, all summer storms were dominated by old water. Storms in a neighboring basin were dominated by new water but much less than was the snowmelt event. Thus a large increase in old water contributions occurred following the snowmelt period. This increase continued moderately through the summer in 1994 but not in 1995. We credit the seasonal changes in old water contributions to increased subsurface storage capacity due to thawing of the active layer.
Water Resources Research – Wiley
Published: Jul 1, 1997
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