The Use of Inductive and Deductive Reasoning to Model Snowmelt Runoff from Northern Mountain Catchments

Abstract: Reliable hydrological modeling at small to medium scales is very difficult. At these scale, models require incorporation of both detailed process understanding and inputs along with information gained from observations of basin-wide streamflow phenomenon; essentially a combination of deduc...

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Main Authors: P. F. Dornesa, J. W. Pomeroya, A. Pietronirob, S. K. Careyc, W. L. Quintond
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.4683
http://www.iemss.org/iemss2006/papers/s12/224_Dornes_2.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.547.4683 2023-05-15T17:57:59+02:00 The Use of Inductive and Deductive Reasoning to Model Snowmelt Runoff from Northern Mountain Catchments P. F. Dornesa J. W. Pomeroya A. Pietronirob S. K. Careyc W. L. Quintond The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.4683 http://www.iemss.org/iemss2006/papers/s12/224_Dornes_2.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.4683 http://www.iemss.org/iemss2006/papers/s12/224_Dornes_2.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.iemss.org/iemss2006/papers/s12/224_Dornes_2.pdf text ftciteseerx 2016-01-08T11:21:19Z Abstract: Reliable hydrological modeling at small to medium scales is very difficult. At these scale, models require incorporation of both detailed process understanding and inputs along with information gained from observations of basin-wide streamflow phenomenon; essentially a combination of deductive and inductive approaches. At Granger Creek, part of the Wolf Creek Research Basin in the mountains of the Yukon Territory, Canada, sparse and shrub tundra cover the basin and soils are frozen at the time of snowmelt. Wind redistributes snow to north facing slopes and shrub tundra areas, while spring melt rates are much higher on south facing slopes due to increased incident solar radiation. Soil moisture and porosity are higher on north facing slopes and notably smaller on south facing slopes, reflecting cumulative differences in summer evaporation losses and the presence of permafrost on north slopes. Observations of streamflow show that peak flows are due to snowmelt, and that the timing of the peak is associated with the timing of snowmelt in the shrub-tundra vegetation zone, while the duration of the peak is associated with the duration of snowmelt on north facing slopes and high elevation zones. Despite small scale observations of rapid and early snowmelt on the south facing slopes, melt from these slopes occurs well before the spring hydrograph rise. To incorporate information from our recent advances in process understanding and in basin streamflow behavior, a ‘hydrological response ’ landscape unit modeling approach is used including information on: Text permafrost Tundra Yukon Unknown Yukon Canada Granger Creek ENVELOPE(-123.303,-123.303,57.600,57.600)
institution Open Polar
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language English
description Abstract: Reliable hydrological modeling at small to medium scales is very difficult. At these scale, models require incorporation of both detailed process understanding and inputs along with information gained from observations of basin-wide streamflow phenomenon; essentially a combination of deductive and inductive approaches. At Granger Creek, part of the Wolf Creek Research Basin in the mountains of the Yukon Territory, Canada, sparse and shrub tundra cover the basin and soils are frozen at the time of snowmelt. Wind redistributes snow to north facing slopes and shrub tundra areas, while spring melt rates are much higher on south facing slopes due to increased incident solar radiation. Soil moisture and porosity are higher on north facing slopes and notably smaller on south facing slopes, reflecting cumulative differences in summer evaporation losses and the presence of permafrost on north slopes. Observations of streamflow show that peak flows are due to snowmelt, and that the timing of the peak is associated with the timing of snowmelt in the shrub-tundra vegetation zone, while the duration of the peak is associated with the duration of snowmelt on north facing slopes and high elevation zones. Despite small scale observations of rapid and early snowmelt on the south facing slopes, melt from these slopes occurs well before the spring hydrograph rise. To incorporate information from our recent advances in process understanding and in basin streamflow behavior, a ‘hydrological response ’ landscape unit modeling approach is used including information on:
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author P. F. Dornesa
J. W. Pomeroya
A. Pietronirob
S. K. Careyc
W. L. Quintond
spellingShingle P. F. Dornesa
J. W. Pomeroya
A. Pietronirob
S. K. Careyc
W. L. Quintond
The Use of Inductive and Deductive Reasoning to Model Snowmelt Runoff from Northern Mountain Catchments
author_facet P. F. Dornesa
J. W. Pomeroya
A. Pietronirob
S. K. Careyc
W. L. Quintond
author_sort P. F. Dornesa
title The Use of Inductive and Deductive Reasoning to Model Snowmelt Runoff from Northern Mountain Catchments
title_short The Use of Inductive and Deductive Reasoning to Model Snowmelt Runoff from Northern Mountain Catchments
title_full The Use of Inductive and Deductive Reasoning to Model Snowmelt Runoff from Northern Mountain Catchments
title_fullStr The Use of Inductive and Deductive Reasoning to Model Snowmelt Runoff from Northern Mountain Catchments
title_full_unstemmed The Use of Inductive and Deductive Reasoning to Model Snowmelt Runoff from Northern Mountain Catchments
title_sort use of inductive and deductive reasoning to model snowmelt runoff from northern mountain catchments
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.4683
http://www.iemss.org/iemss2006/papers/s12/224_Dornes_2.pdf
long_lat ENVELOPE(-123.303,-123.303,57.600,57.600)
geographic Yukon
Canada
Granger Creek
geographic_facet Yukon
Canada
Granger Creek
genre permafrost
Tundra
Yukon
genre_facet permafrost
Tundra
Yukon
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http://www.iemss.org/iemss2006/papers/s12/224_Dornes_2.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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