Timing, progression, duration: an investigation of temporal patterns of break-up and ice jam flooding in the Mackenzie Delta, NWT
The Mackenzie Delta is covered in freshwater lakes that provide habitat for a myriad of species. The hydrology of these delta lakes is dominated by cryospheric processes, specifically snowmelt induced spring break-up ice jams, which typically produce the largest hydrologic event of the year. In ligh...
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ftwestwashington:oai:cedar.wwu.edu:wdcag-1039 2023-05-15T17:09:28+02:00 Timing, progression, duration: an investigation of temporal patterns of break-up and ice jam flooding in the Mackenzie Delta, NWT Goulding, Holly L. 2008-03-08T16:00:00Z https://cedar.wwu.edu/wdcag/2008wdcag/2008/40 English eng Western CEDAR https://cedar.wwu.edu/wdcag/2008wdcag/2008/40 Copying of this document in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this document for commercial purposes, or for financial gain, shall not be allowed without the author's written permission. Western Division, Canadian Association of Geographers river-ice break-up floods temporal patterns Mackenzie Delta Geography text 2008 ftwestwashington 2022-09-14T05:54:28Z The Mackenzie Delta is covered in freshwater lakes that provide habitat for a myriad of species. The hydrology of these delta lakes is dominated by cryospheric processes, specifically snowmelt induced spring break-up ice jams, which typically produce the largest hydrologic event of the year. In light of limited current understanding of break-up patterns and processes in the delta, the objective of this research is to explore the temporal variability of break-up and ice-affected extreme floods in the delta. Data gathered from a variety of sources, including hydrometric and meteorological stations, radar and satellite imagery, air photography, and historical observations, are assembled to create a break-up chronology for the delta. This includes an index of the timing of initiation of pronounced spring melting, as well as the initiation of break-up, the peak break-up water level, and the last day of ice effects for 15 Water Survey of Canada hydrometric stations in the Mackenzie Delta over the period from 1972 to 2006. Within the subset of identified extreme flood years, distinct timing patterns emerge, which can ultimately be linked to dominant hydroclimatic influences. These findings are part of the first stage of an ongoing investigation into the hydroclimatic controls on extreme hydrological events in the Mackenzie Delta. Text Mackenzie Delta Western Washington University: CEDAR (Contributing to Education through Digital Access to Research) Canada Mackenzie Delta ENVELOPE(-136.672,-136.672,68.833,68.833) |
institution |
Open Polar |
collection |
Western Washington University: CEDAR (Contributing to Education through Digital Access to Research) |
op_collection_id |
ftwestwashington |
language |
English |
topic |
river-ice break-up floods temporal patterns Mackenzie Delta Geography |
spellingShingle |
river-ice break-up floods temporal patterns Mackenzie Delta Geography Goulding, Holly L. Timing, progression, duration: an investigation of temporal patterns of break-up and ice jam flooding in the Mackenzie Delta, NWT |
topic_facet |
river-ice break-up floods temporal patterns Mackenzie Delta Geography |
description |
The Mackenzie Delta is covered in freshwater lakes that provide habitat for a myriad of species. The hydrology of these delta lakes is dominated by cryospheric processes, specifically snowmelt induced spring break-up ice jams, which typically produce the largest hydrologic event of the year. In light of limited current understanding of break-up patterns and processes in the delta, the objective of this research is to explore the temporal variability of break-up and ice-affected extreme floods in the delta. Data gathered from a variety of sources, including hydrometric and meteorological stations, radar and satellite imagery, air photography, and historical observations, are assembled to create a break-up chronology for the delta. This includes an index of the timing of initiation of pronounced spring melting, as well as the initiation of break-up, the peak break-up water level, and the last day of ice effects for 15 Water Survey of Canada hydrometric stations in the Mackenzie Delta over the period from 1972 to 2006. Within the subset of identified extreme flood years, distinct timing patterns emerge, which can ultimately be linked to dominant hydroclimatic influences. These findings are part of the first stage of an ongoing investigation into the hydroclimatic controls on extreme hydrological events in the Mackenzie Delta. |
format |
Text |
author |
Goulding, Holly L. |
author_facet |
Goulding, Holly L. |
author_sort |
Goulding, Holly L. |
title |
Timing, progression, duration: an investigation of temporal patterns of break-up and ice jam flooding in the Mackenzie Delta, NWT |
title_short |
Timing, progression, duration: an investigation of temporal patterns of break-up and ice jam flooding in the Mackenzie Delta, NWT |
title_full |
Timing, progression, duration: an investigation of temporal patterns of break-up and ice jam flooding in the Mackenzie Delta, NWT |
title_fullStr |
Timing, progression, duration: an investigation of temporal patterns of break-up and ice jam flooding in the Mackenzie Delta, NWT |
title_full_unstemmed |
Timing, progression, duration: an investigation of temporal patterns of break-up and ice jam flooding in the Mackenzie Delta, NWT |
title_sort |
timing, progression, duration: an investigation of temporal patterns of break-up and ice jam flooding in the mackenzie delta, nwt |
publisher |
Western CEDAR |
publishDate |
2008 |
url |
https://cedar.wwu.edu/wdcag/2008wdcag/2008/40 |
long_lat |
ENVELOPE(-136.672,-136.672,68.833,68.833) |
geographic |
Canada Mackenzie Delta |
geographic_facet |
Canada Mackenzie Delta |
genre |
Mackenzie Delta |
genre_facet |
Mackenzie Delta |
op_source |
Western Division, Canadian Association of Geographers |
op_relation |
https://cedar.wwu.edu/wdcag/2008wdcag/2008/40 |
op_rights |
Copying of this document in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this document for commercial purposes, or for financial gain, shall not be allowed without the author's written permission. |
_version_ |
1766065577276735488 |