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Record W7133087266

A Critical Analysis of the Adjustment of River Channel Geometry in Southern Ontario and the Role of Land Use, Climate Variability, and Boundary Conditions

2024· dissertation· W7133087266 on OpenAlexaboutno aff
Pamela E. Tetford

Bibliographic record

VenueTSpace · 2024
Typedissertation
Language
FieldEnvironmental Science
TopicHydrology and Sediment Transport Processes
Canadian institutionsnot available
Fundersnot available
KeywordsAggradationHydrology (agriculture)Flood mythChannel (broadcasting)Drainage basinStreamflowErosionPrecipitationDisturbance (geology)Surface runoff
DOInot available

Abstract

fetched live from OpenAlex

Self-shaping alluvial river channels attempt to adjust their geometry to allow just enough flow velocity to transport sediment, without aggradation or degradation. However, hydrological settings influence river responsiveness. This study investigates the morphodynamic response of semi-alluvial rivers to land use modification in southern Ontario to better understand the relationships between streamflow and channel self-adjustment in deglaciated regions. Analysis considers hydrologic controls on flood frequency, a determination of “effective” flow, and inadvertent experimentation examining the morphological responses of three semi-alluvial rivers distinguished by the degree of urbanization. Identifying a formative channel discharge is paramount. There is no single “best fit” statistical distribution type to model annual maximum gauge data in southern Ontario due to hydrologic variability. Precipitation is a greater predictor of more frequent, low-magnitude floods whereas surficial geology has more predictive value for less frequent, high-magnitude events. Over a broad range of flood recurrence intervals, a zonal two-variable model accounting for drainage area and the percentage of naturalized land use that accounts for surface water storage, significantly improves flood prediction. Moderate- to high-levels of land use disturbance produce disproportionately low channel width-to-depth ratios, likely due to human intervention. Tilled cropping leads to enlargement of headwater channels resulting from flashy overland flow. Low disturbance headwater channels widen in response to higher stream energy when descending from glacial moraine deposits that are more susceptible to erosion from wet/dry cycles. In southern Ontario, continued shifts in seasonal flood occurrence due to climate warming will increase midwinter freeze/thaw cycles on till beds/banks, furthering channel instability. In urbanizing rivers with erodible till banks, engineering/intervention that produces straighter, steeper channels with limited sediment supply generates channel widening (where possible) in response to increased stream energy. Self-adjusting channels increase their sinuosity and replenish bedload, producing less widening. Where channel restoration is necessary, channels lined by deep-rooted trees better resist migration than those lined by shallow-rooted pioneer species. Assessment of land use disturbance leading to channel enlargement can be accomplished using LiDAR data coupled with an applied river channel regime model. Model results efficiently predict channel geometry in the absence of urbanization to characterise “natural” stream channels.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.039
Threshold uncertainty score0.080

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.008
GPT teacher head0.264
Teacher spread0.256 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2024
Admission routes1
Has abstractyes

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