Determining Hillslope Diffusion Rates in a Boreal Forest: Quaternary Fluvial Terraces in the Nenana River Valley, Central Alaska Range
The subarctic boreal forest biome is predicted to experience higher magnitudes of warming than other biomes due to climate change. The effects of this warming will be pronounced in areas underlain by discontinuous permafrost where melting permafrost and distinct changes in vegetation patterns are ex...
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ftunivkentucky:oai:uknowledge.uky.edu:ees_etds-1018 2023-05-15T13:09:36+02:00 Determining Hillslope Diffusion Rates in a Boreal Forest: Quaternary Fluvial Terraces in the Nenana River Valley, Central Alaska Range Walker, Laurel Anne 2014-01-01T08:00:00Z application/pdf https://uknowledge.uky.edu/ees_etds/16 https://uknowledge.uky.edu/cgi/viewcontent.cgi?article=1018&context=ees_etds unknown UKnowledge https://uknowledge.uky.edu/ees_etds/16 https://uknowledge.uky.edu/cgi/viewcontent.cgi?article=1018&context=ees_etds Theses and Dissertations--Earth and Environmental Sciences Alaska Range Nenana River Valley Boreal Forest Hillslope Diffusion Quartz Optically Stimulated Luminescence Geology Geomorphology Other Earth Sciences Sedimentology Soil Science Tectonics and Structure text 2014 ftunivkentucky 2021-08-29T18:19:54Z The subarctic boreal forest biome is predicted to experience higher magnitudes of warming than other biomes due to climate change. The effects of this warming will be pronounced in areas underlain by discontinuous permafrost where melting permafrost and distinct changes in vegetation patterns are expected. To better understand rates of hillslope diffusion in the boreal forest I have used a geomorphic process modeling approach, using data from a sequence of Quaternary fluvial terraces located in the Nenana River valley of central Alaska. I hypothesized that diffusion rates here would be slower when compared to the mid-latitudes, and faster on north versus south-facing slopes. Calculated diffusion rates do support the hypothesis as they fall on the lower end of the global spectrum of documented hillslope diffusion rates. However, a significant difference in diffusion rates is not seen between the predominantly northeast and southwest facing slopes used in this study. Text alaska range permafrost Subarctic Alaska University of Kentucky: UKnowledge |
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University of Kentucky: UKnowledge |
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ftunivkentucky |
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topic |
Alaska Range Nenana River Valley Boreal Forest Hillslope Diffusion Quartz Optically Stimulated Luminescence Geology Geomorphology Other Earth Sciences Sedimentology Soil Science Tectonics and Structure |
spellingShingle |
Alaska Range Nenana River Valley Boreal Forest Hillslope Diffusion Quartz Optically Stimulated Luminescence Geology Geomorphology Other Earth Sciences Sedimentology Soil Science Tectonics and Structure Walker, Laurel Anne Determining Hillslope Diffusion Rates in a Boreal Forest: Quaternary Fluvial Terraces in the Nenana River Valley, Central Alaska Range |
topic_facet |
Alaska Range Nenana River Valley Boreal Forest Hillslope Diffusion Quartz Optically Stimulated Luminescence Geology Geomorphology Other Earth Sciences Sedimentology Soil Science Tectonics and Structure |
description |
The subarctic boreal forest biome is predicted to experience higher magnitudes of warming than other biomes due to climate change. The effects of this warming will be pronounced in areas underlain by discontinuous permafrost where melting permafrost and distinct changes in vegetation patterns are expected. To better understand rates of hillslope diffusion in the boreal forest I have used a geomorphic process modeling approach, using data from a sequence of Quaternary fluvial terraces located in the Nenana River valley of central Alaska. I hypothesized that diffusion rates here would be slower when compared to the mid-latitudes, and faster on north versus south-facing slopes. Calculated diffusion rates do support the hypothesis as they fall on the lower end of the global spectrum of documented hillslope diffusion rates. However, a significant difference in diffusion rates is not seen between the predominantly northeast and southwest facing slopes used in this study. |
format |
Text |
author |
Walker, Laurel Anne |
author_facet |
Walker, Laurel Anne |
author_sort |
Walker, Laurel Anne |
title |
Determining Hillslope Diffusion Rates in a Boreal Forest: Quaternary Fluvial Terraces in the Nenana River Valley, Central Alaska Range |
title_short |
Determining Hillslope Diffusion Rates in a Boreal Forest: Quaternary Fluvial Terraces in the Nenana River Valley, Central Alaska Range |
title_full |
Determining Hillslope Diffusion Rates in a Boreal Forest: Quaternary Fluvial Terraces in the Nenana River Valley, Central Alaska Range |
title_fullStr |
Determining Hillslope Diffusion Rates in a Boreal Forest: Quaternary Fluvial Terraces in the Nenana River Valley, Central Alaska Range |
title_full_unstemmed |
Determining Hillslope Diffusion Rates in a Boreal Forest: Quaternary Fluvial Terraces in the Nenana River Valley, Central Alaska Range |
title_sort |
determining hillslope diffusion rates in a boreal forest: quaternary fluvial terraces in the nenana river valley, central alaska range |
publisher |
UKnowledge |
publishDate |
2014 |
url |
https://uknowledge.uky.edu/ees_etds/16 https://uknowledge.uky.edu/cgi/viewcontent.cgi?article=1018&context=ees_etds |
genre |
alaska range permafrost Subarctic Alaska |
genre_facet |
alaska range permafrost Subarctic Alaska |
op_source |
Theses and Dissertations--Earth and Environmental Sciences |
op_relation |
https://uknowledge.uky.edu/ees_etds/16 https://uknowledge.uky.edu/cgi/viewcontent.cgi?article=1018&context=ees_etds |
_version_ |
1766189775463645184 |