- Library Home /
- Search Collections /
- Open Collections /
- Browse Collections /
- UBC Theses and Dissertations /
- Stratification during spring and summer in a brackish...
Open Collections
UBC Theses and Dissertations
UBC Theses and Dissertations
Stratification during spring and summer in a brackish lake subject to ice cover Jamali, Sara
Abstract
In recent decades temperate lakes have experienced notable changes in their thermal regimes, including extended durations of summer stratification and shorter ice-covered periods. In addition, recent studies have shown that the presence of low levels of salinity can have dramatic effects on the circulation of ice-covered lakes. For example, the exclusion of salt from ice as it forms can result in a relatively fresh surface layer immediately after ice melt. The density contrast between the ice-melt and the more saline water beneath it can be sufficient to hinder, or even prevent, turnover. These changes have far-reaching ecological consequences, influencing oxygen availability, nutrient cycling, and biological productivity. Base Mine Lake Demonstration (BML) in Alberta, Canada (57°1'N, 111°37'W) is the first full-scale demonstration of an end pit lake in the oil sands industry. BML was formed by the backfilling of a previously mined-out pit with fluid fine tailings, followed by the addition of fresh water from a nearby reservoir. The evolution of the resulting brackish lake has been actively monitored since its commissioning in 2012. In the present study we investigate the inhibition and dynamics of spring turnover, and the establishment of summer stratification, in BML. Field observations from spring and summer of 2016 and 2017 are analyzed using a conceptual model, and compared with simulations from the one-dimensional General Lake Model (GLM), to assess changes in the temperature stratification during notable wind events. Results indicate that although significant mixing occurs after ice-off, complete turnover is not achieved; instead, the lake experiences long periods of upwelling/downwelling and short periods (hours) of partial spring turnover. Additionally, the dynamics at BML are influenced by the expression of saline pore water from the settling of the underlying tailings. These findings highlight both the complex mixing dynamics within BML and the limitations of using a one-dimensional model to represent this system.
Item Metadata
Title |
Stratification during spring and summer in a brackish lake subject to ice cover
|
Creator | |
Supervisor | |
Publisher |
University of British Columbia
|
Date Issued |
2025
|
Description |
In recent decades temperate lakes have experienced notable changes in their thermal regimes,
including extended durations of summer stratification and shorter ice-covered periods. In addition, recent studies have shown that the presence of low levels of salinity can have dramatic
effects on the circulation of ice-covered lakes. For example, the exclusion of salt from ice as
it forms can result in a relatively fresh surface layer immediately after ice melt. The density
contrast between the ice-melt and the more saline water beneath it can be sufficient to hinder,
or even prevent, turnover. These changes have far-reaching ecological consequences, influencing
oxygen availability, nutrient cycling, and biological productivity.
Base Mine Lake Demonstration (BML) in Alberta, Canada (57°1'N, 111°37'W) is the first
full-scale demonstration of an end pit lake in the oil sands industry. BML was formed by the
backfilling of a previously mined-out pit with fluid fine tailings, followed by the addition of fresh
water from a nearby reservoir. The evolution of the resulting brackish lake has been actively
monitored since its commissioning in 2012.
In the present study we investigate the inhibition and dynamics of spring turnover, and the
establishment of summer stratification, in BML. Field observations from spring and summer
of 2016 and 2017 are analyzed using a conceptual model, and compared with simulations from
the one-dimensional General Lake Model (GLM), to assess changes in the temperature stratification during notable wind events. Results indicate that although significant mixing occurs
after ice-off, complete turnover is not achieved; instead, the lake experiences long periods of
upwelling/downwelling and short periods (hours) of partial spring turnover. Additionally, the
dynamics at BML are influenced by the expression of saline pore water from the settling of the
underlying tailings. These findings highlight both the complex mixing dynamics within BML
and the limitations of using a one-dimensional model to represent this system.
|
Genre | |
Type | |
Language |
eng
|
Date Available |
2025-09-08
|
Provider |
Vancouver : University of British Columbia Library
|
Rights |
Attribution-NonCommercial-NoDerivatives 4.0 International
|
DOI |
10.14288/1.0450074
|
URI | |
Degree (Theses) | |
Program (Theses) | |
Affiliation | |
Degree Grantor |
University of British Columbia
|
Graduation Date |
2025-11
|
Campus | |
Scholarly Level |
Graduate
|
Rights URI | |
Aggregated Source Repository |
DSpace
|
Item Media
Item Citations and Data
Rights
Attribution-NonCommercial-NoDerivatives 4.0 International