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Record W4408427932 · doi:10.5194/egusphere-egu25-12669

Hydrodynamic Modelling of Great Slave Lake Using NEMO

2025· preprint· en· W4408427932 on OpenAlexaffabout
Jonas Stankevicius, Alain Pietroniro, Qi Zhou

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEarth and Planetary Sciences
TopicAquatic and Environmental Studies
Canadian institutionsUniversity of Calgary
Fundersnot available
KeywordsEnvironmental scienceHydrology (agriculture)GeologyGeotechnical engineering

Abstract

fetched live from OpenAlex

The subarctic region of northern Canada, including the Mackenzie River basin is deeply impacted by the changing climate. Unprecedented rates of warming in Canada’s North, up to four times the global average, have been observed in the region over the past few decades. This brings significant implications for regional hydrology, ecosystems, and human activities. A major controlling feature in the Mackenzie River Basin is Great Slave Lake, which is the second largest lake in the Northwest Territories of Canada and the deepest lake in North America. With over 60% of the population of Northwest Territories living along its shores, Great Slave Lake is a vital ecological and societal asset in the region. This study aims to further our understanding of water circulation and stratification patterns in Great Slave Lake through numerical simulation. Despite the status of Great Slave Lake as one of the largest and deepest lakes in North America, comprehensive numerical modelling has proven difficult due to lack of accurate bathymetric data. To address this gap, we collaborated with the Department of Fisheries and Oceans to develop the first complete bathymetric map of Great Slave Lake. Historical naval charts and field sheets were integrated with additional sounding data to produce a simulation domain tailored to the Nucleus for European Modelling of the Ocean (NEMO) at a horizontal resolution of 1km with 30 vertical layers. The NEMO model was chosen for application in this large lake for consistency with the existing model setup being used by Environment and Climate Change Canada (ECCC) for its operational forecasting system in the Laurentian Great Lakes. Atmospheric reanalysis is provided by ECCC’S Regional Deterministic Reanalysis System (RDRS), while surface runoff entering the lake is driven by the Community Environmental Modelling System – Surface & Hydrology (MESH) outputs from the Global Water Futures reanalysis efforts. The resulting NEMO model shows good capability of simulating lake processes with preliminary results indicating that the lake exhibits seasonal thermal stratification, consistent with dimictic behaviour, where full vertical mixing occurs twice annually. Our results also show that wind-induced mixing appears to also play a significant role in lake circulation, and a counterclockwise circulation pattern is observed, with prominent gyres in the main basin of the lake. Ongoing work focuses on further validation of the temperature profiles at select locations and sensitivity analysis to improve the overall simulation capabilities of the model for future water resource management needs.

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.247
Threshold uncertainty score0.998

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.049
GPT teacher head0.220
Teacher spread0.172 · 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 teacher head, not a consensus.

Study designSimulation or modeling
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
Published2025
Admission routes2
Has abstractyes

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