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Record W2132983843 · doi:10.1002/hyp.7409

Glacier contribution to the North and South Saskatchewan Rivers

2009· article· en· W2132983843 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.
fundA Canadian funder is recorded on the work.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.

Bibliographic record

VenueHydrological Processes · 2009
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicCryospheric studies and observations
Canadian institutionsGeological Survey of CanadaNatural Resources CanadaEnvironment and Climate Change CanadaUniversity of Saskatchewan
FundersNatural Resources CanadaCanadian Foundation for Climate and Atmospheric Sciences
KeywordsGlacierSnowmeltMeltwaterStreamflowSnowHydrology (agriculture)HydrographSurface runoffDrainage basinWater yearGeologyClimatologyEnvironmental scienceStructural basinGlacier mass balancePhysical geographyGeomorphologyGeography

Abstract

fetched live from OpenAlex

Abstract The hydrological model WATFLOOD and a separate volume–area scaling relationship are applied to estimate glacier wastage and seasonal Melt contribution to the North and South Saskatchewan Rivers originating in the Canadian Rocky Mountains (1975–1998). Wastage is the ice melt volume that exceeds the volume of snow accumulation into the glacier system in a hydrological year, causing an annual net loss of glacier volume. Melt is the ice melt volume that is equal to, or less than, the volume of snow that accumulates into the glacier system in a hydrological year. By our definition then, glacier Melt is a storage term and does not contribute to increased total annual streamflow. Water is stored as snow on accumulation into the glacier system, and the water equivalent runoff is delayed until ice melts in the late summer months of the otherwise low streamflow. Wastage varied between basins with similar glacierized areas reflecting the individual response of glaciers to climate, contributing over 10% to July‐to‐September streamflow in some headwater basins, but under 3% annually to the regulated flow at Edmonton and Calgary. Melt was positively correlated with basin glacierized area and contributed over 27% to July‐to‐September flow from basins with greater than 1% glacierized area, and over double the wastage volume at Edmonton and Calgary. Future glacier decline is therefore expected to result mainly in an advancement of peak flow towards a non‐glacierized snowmelt regime hydrograph, resulting in significantly reduced late summer flows further reduced by decreasing wastage contributions. Copyright © 2009 John Wiley & Sons, Ltd and Her Majesty the Queen in right of Canada.

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.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.023
Threshold uncertainty score0.260

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)0.0000.000

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 head0.016
GPT teacher head0.205
Teacher spread0.189 · 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