Permafrost development and active-layer hydrology of peat plateaus in wetland-dominated discontinuous permafrost ...
In the wetland dominated discontinuous permafrost of the Canadian sub-artic, hydrological processes are governed by permafrost and active layer development associated with different landcover types. Subsurface runoff from the mosaic of different landcover types in the Scotty Creek research basin, No...
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2014
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Online Access: | https://dx.doi.org/10.11575/prism/27308 https://prism.ucalgary.ca/handle/11023/1410 |
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ftdatacite:10.11575/prism/27308 2023-11-05T03:44:21+01:00 Permafrost development and active-layer hydrology of peat plateaus in wetland-dominated discontinuous permafrost ... Christensen, Brendan 2014 https://dx.doi.org/10.11575/prism/27308 https://prism.ucalgary.ca/handle/11023/1410 en eng Graduate Studies University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Hydrology Engineering--Environmental Permafrost subarctic Peatlands Runoff Active-layer article master thesis CreativeWork Other 2014 ftdatacite https://doi.org/10.11575/prism/27308 2023-10-09T10:52:24Z In the wetland dominated discontinuous permafrost of the Canadian sub-artic, hydrological processes are governed by permafrost and active layer development associated with different landcover types. Subsurface runoff from the mosaic of different landcover types in the Scotty Creek research basin, Northwest Territories, Canada, is governed by permafrost cored peat plateaus that are elevated above surrounding bogs and fens. To predict how runoff from peat plateaus in this environment may be changing as permafrost freeze-thaw processes evolve under changing physical and climatic conditions, a model accounting for surface and soil freeze-thaw processes and lateral runoff from simplified peat plateaus is developed. This model utilizes the Northern Ecosystem Soil Temperature (NEST) model to simulate surface and soil freeze-thaw processes by solving the surface energy balance and soil heat conduction equation. As runoff processes from NEST are not physically based, the Simple Fill And Spill Hydrology (SFASH) model, ... Master Thesis Northwest Territories Peat permafrost Subarctic DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Hydrology Engineering--Environmental Permafrost subarctic Peatlands Runoff Active-layer |
spellingShingle |
Hydrology Engineering--Environmental Permafrost subarctic Peatlands Runoff Active-layer Christensen, Brendan Permafrost development and active-layer hydrology of peat plateaus in wetland-dominated discontinuous permafrost ... |
topic_facet |
Hydrology Engineering--Environmental Permafrost subarctic Peatlands Runoff Active-layer |
description |
In the wetland dominated discontinuous permafrost of the Canadian sub-artic, hydrological processes are governed by permafrost and active layer development associated with different landcover types. Subsurface runoff from the mosaic of different landcover types in the Scotty Creek research basin, Northwest Territories, Canada, is governed by permafrost cored peat plateaus that are elevated above surrounding bogs and fens. To predict how runoff from peat plateaus in this environment may be changing as permafrost freeze-thaw processes evolve under changing physical and climatic conditions, a model accounting for surface and soil freeze-thaw processes and lateral runoff from simplified peat plateaus is developed. This model utilizes the Northern Ecosystem Soil Temperature (NEST) model to simulate surface and soil freeze-thaw processes by solving the surface energy balance and soil heat conduction equation. As runoff processes from NEST are not physically based, the Simple Fill And Spill Hydrology (SFASH) model, ... |
format |
Master Thesis |
author |
Christensen, Brendan |
author_facet |
Christensen, Brendan |
author_sort |
Christensen, Brendan |
title |
Permafrost development and active-layer hydrology of peat plateaus in wetland-dominated discontinuous permafrost ... |
title_short |
Permafrost development and active-layer hydrology of peat plateaus in wetland-dominated discontinuous permafrost ... |
title_full |
Permafrost development and active-layer hydrology of peat plateaus in wetland-dominated discontinuous permafrost ... |
title_fullStr |
Permafrost development and active-layer hydrology of peat plateaus in wetland-dominated discontinuous permafrost ... |
title_full_unstemmed |
Permafrost development and active-layer hydrology of peat plateaus in wetland-dominated discontinuous permafrost ... |
title_sort |
permafrost development and active-layer hydrology of peat plateaus in wetland-dominated discontinuous permafrost ... |
publisher |
Graduate Studies |
publishDate |
2014 |
url |
https://dx.doi.org/10.11575/prism/27308 https://prism.ucalgary.ca/handle/11023/1410 |
genre |
Northwest Territories Peat permafrost Subarctic |
genre_facet |
Northwest Territories Peat permafrost Subarctic |
op_rights |
University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. |
op_doi |
https://doi.org/10.11575/prism/27308 |
_version_ |
1781704025659408384 |