Slope Hydroclimatology and Hydrologic Responses to Global Change in a Small High Arctic Basin

This study evaluated the present-day interactions between the atmosphere, soils, water flow and vegetation patterns of a remote area of Northern Canada. This study showed that microclimatic processes (temperature, radiation) are often the driving force behind snowmelt and ground thaw. This study als...

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Bibliographic Details
Main Author: Young, Kathy L.
Other Authors: Woo, M.K., Geography
Format: Thesis
Language:unknown
Published: 2010
Subjects:
Online Access:http://hdl.handle.net/11375/7077
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spelling ftmcmaster:oai:macsphere.mcmaster.ca:11375/7077 2024-09-15T17:52:14+00:00 Slope Hydroclimatology and Hydrologic Responses to Global Change in a Small High Arctic Basin Young, Kathy L. Woo, M.K. Geography 2010-06-29 http://hdl.handle.net/11375/7077 unknown opendissertations/2373 3357 1375737 http://hdl.handle.net/11375/7077 Geography thesis 2010 ftmcmaster 2024-06-26T04:35:24Z This study evaluated the present-day interactions between the atmosphere, soils, water flow and vegetation patterns of a remote area of Northern Canada. This study showed that microclimatic processes (temperature, radiation) are often the driving force behind snowmelt and ground thaw. This study also showed that it was possible to use limited field camp data (e.g. 2x daily cloud, temperature, wind) to simulate radiation and energy fluxes for a variety of surfaces. This suggests the model's utility by cologists and earth scientists working in other areas of the Arctic. This thesis also showed that it was possible to use point data to simulate melt and evaporation for a small High Arctic basin and to investigate some possible implications of climate change to water movement. This last stage of the study will be particularly relevant to climatologists, ecologists and geomorphologists working in the north. Doctor of Philosophy (PhD) Thesis Arctic Basin Climate change MacSphere (McMaster University)
institution Open Polar
collection MacSphere (McMaster University)
op_collection_id ftmcmaster
language unknown
topic Geography
spellingShingle Geography
Young, Kathy L.
Slope Hydroclimatology and Hydrologic Responses to Global Change in a Small High Arctic Basin
topic_facet Geography
description This study evaluated the present-day interactions between the atmosphere, soils, water flow and vegetation patterns of a remote area of Northern Canada. This study showed that microclimatic processes (temperature, radiation) are often the driving force behind snowmelt and ground thaw. This study also showed that it was possible to use limited field camp data (e.g. 2x daily cloud, temperature, wind) to simulate radiation and energy fluxes for a variety of surfaces. This suggests the model's utility by cologists and earth scientists working in other areas of the Arctic. This thesis also showed that it was possible to use point data to simulate melt and evaporation for a small High Arctic basin and to investigate some possible implications of climate change to water movement. This last stage of the study will be particularly relevant to climatologists, ecologists and geomorphologists working in the north. Doctor of Philosophy (PhD)
author2 Woo, M.K.
Geography
format Thesis
author Young, Kathy L.
author_facet Young, Kathy L.
author_sort Young, Kathy L.
title Slope Hydroclimatology and Hydrologic Responses to Global Change in a Small High Arctic Basin
title_short Slope Hydroclimatology and Hydrologic Responses to Global Change in a Small High Arctic Basin
title_full Slope Hydroclimatology and Hydrologic Responses to Global Change in a Small High Arctic Basin
title_fullStr Slope Hydroclimatology and Hydrologic Responses to Global Change in a Small High Arctic Basin
title_full_unstemmed Slope Hydroclimatology and Hydrologic Responses to Global Change in a Small High Arctic Basin
title_sort slope hydroclimatology and hydrologic responses to global change in a small high arctic basin
publishDate 2010
url http://hdl.handle.net/11375/7077
genre Arctic Basin
Climate change
genre_facet Arctic Basin
Climate change
op_relation opendissertations/2373
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1375737
http://hdl.handle.net/11375/7077
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