Hydrologic control on proglacial suspended sediment dynamics

Measuring suspended sediment concentration (SSC) is both costly and labour intensive. Temporal records of SSC are, however, of paramount importance in elucidating issues relating to geomorphology, ecology and water quality. Rating curves, that relate SSC and discharge by a simple linear regressio...

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Main Author: Richards, George
Format: Others
Language:English
Published: 2009
Online Access:http://hdl.handle.net/2429/11827
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spelling ndltd-UBC-oai-circle.library.ubc.ca-2429-118272018-01-05T17:36:07Z Hydrologic control on proglacial suspended sediment dynamics Richards, George Measuring suspended sediment concentration (SSC) is both costly and labour intensive. Temporal records of SSC are, however, of paramount importance in elucidating issues relating to geomorphology, ecology and water quality. Rating curves, that relate SSC and discharge by a simple linear regression function, are frequently employed by workers to address the problems of recording SSC. Such functions, however, rarely account for more than 50% of the variability in observed SSC. The aim of this thesis is to formulate subseasonal predictive SSC models and to investigate hydrologic controls on proglacial suspended sediment dynamics using data collected from a glacier-fed stream, Coast Mountains, British Columbia. In order to model proglacial SSC, the hydrologic season was initially divided into nival, nival-glacial, glacial and autumn recession periods, according to sudden shifts in the ratio of stream discharge between the glacierised and a neighbouring unglacierised catchment of similar size and aspect. Multiple regression functions, to predict SSC, were then developed for each period. These regression models incorporate a suite of easily measured variables and are shown to reduce significantly, initial problems of autocorrelation, heteroskedasticity and non-linearity of the SSC-discharge relationship. Analysis of the significant parameters in the multiple regression models, the hysteretic relationship between SSC and discharge, and downstream changes in SSC reveal that short-term, within channel, storage of fine sediment may be an important control on proglacial suspended sediment dynamics in this complex glaciofluvial lacustrine system. Arts, Faculty of Geography, Department of Graduate 2009-08-06 2009-08-06 2001 2001-11 Text Thesis/Dissertation http://hdl.handle.net/2429/11827 eng For non-commercial purposes only, such as research, private study and education. Additional conditions apply, see Terms of Use https://open.library.ubc.ca/terms_of_use. 6255961 bytes application/pdf
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language English
format Others
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description Measuring suspended sediment concentration (SSC) is both costly and labour intensive. Temporal records of SSC are, however, of paramount importance in elucidating issues relating to geomorphology, ecology and water quality. Rating curves, that relate SSC and discharge by a simple linear regression function, are frequently employed by workers to address the problems of recording SSC. Such functions, however, rarely account for more than 50% of the variability in observed SSC. The aim of this thesis is to formulate subseasonal predictive SSC models and to investigate hydrologic controls on proglacial suspended sediment dynamics using data collected from a glacier-fed stream, Coast Mountains, British Columbia. In order to model proglacial SSC, the hydrologic season was initially divided into nival, nival-glacial, glacial and autumn recession periods, according to sudden shifts in the ratio of stream discharge between the glacierised and a neighbouring unglacierised catchment of similar size and aspect. Multiple regression functions, to predict SSC, were then developed for each period. These regression models incorporate a suite of easily measured variables and are shown to reduce significantly, initial problems of autocorrelation, heteroskedasticity and non-linearity of the SSC-discharge relationship. Analysis of the significant parameters in the multiple regression models, the hysteretic relationship between SSC and discharge, and downstream changes in SSC reveal that short-term, within channel, storage of fine sediment may be an important control on proglacial suspended sediment dynamics in this complex glaciofluvial lacustrine system. === Arts, Faculty of === Geography, Department of === Graduate
author Richards, George
spellingShingle Richards, George
Hydrologic control on proglacial suspended sediment dynamics
author_facet Richards, George
author_sort Richards, George
title Hydrologic control on proglacial suspended sediment dynamics
title_short Hydrologic control on proglacial suspended sediment dynamics
title_full Hydrologic control on proglacial suspended sediment dynamics
title_fullStr Hydrologic control on proglacial suspended sediment dynamics
title_full_unstemmed Hydrologic control on proglacial suspended sediment dynamics
title_sort hydrologic control on proglacial suspended sediment dynamics
publishDate 2009
url http://hdl.handle.net/2429/11827
work_keys_str_mv AT richardsgeorge hydrologiccontrolonproglacialsuspendedsedimentdynamics
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