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Glacial Recession in Cloud Peak Wilderness Area and ...
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Glacial Recession in Cloud Peak Wilderness Area and the Effects on Streamflow
Glacial Recession in Cloud Peak Wilderness Area and the Effects on Streamflow
Name:Personal
Mitchell Fyock Role :Text(marcrelator)
creator
Mitchell Fyock Role :Text(marcrelator)
creator
Name:Personal
Dr. Carl Legleiter Role :Text(marcrelator)
creator
Dr. Carl Legleiter Role :Text(marcrelator)
creator
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Powerpoint/PDF
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Place
Laramie, Wyoming
University of Wyoming (keyDate="yes")
4/24/2010
Laramie, Wyoming
University of Wyoming (keyDate="yes")
4/24/2010
Language:Text
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born digital
abstract
For many rivers in the American Northwest, 50-80% of the annual streamflow is derived from snowmelt predominantly from glaciers. Recent studies have shown that increasing temperatures have caused glaciers to melt earlier in the year, as well as at a faster rate. This is significant because the rate of snowmelt, as well as the date of the peak snow/water equivalent, determines a rivers available water supply later in the water year. By comparing the average date of different rivers peak streamflow to the average date of peak snow/water equivalent various gauging stations; a correlation could be made between the two variables in order to obtain a general trend. The Cloud Peak Glacier underwent seasonal variations, however, a trend was discovered linking earlier dates of peak snow/water equivalent to earlier dates of peak streamflow. This implies that as temperatures increase, the tendency for earlier peak streamflow is occurring. By examining the effects of increased temperature on glacial recession, we can better understand its effects on river systems supported by glacial meltwater. note
From - Undergraduate Research Day 2010 - Celebration of Research - Abstracts
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Undergraduate Research Day
Undergraduate Research Day
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Undergraduate Research Day 2010
Undergraduate Research Day 2010
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http://hdl.handle.net/10176/wyu:543
http://hdl.handle.net/10176/wyu:543
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http://digital.uwyo.edu/copyright.htm
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eng
English :Code(ISO639-2B)
eng