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Record W2102599615 · doi:10.1002/hyp.9383

Changes in the hydrological character of rainfall on the Canadian prairies

2012· article· en· W2102599615 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 · 2012
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicCryospheric studies and observations
Canadian institutionsSaskatoon Medical Imaging
FundersCanadian Foundation for Climate and Atmospheric Sciences
KeywordsSnowpackPrecipitationSurface runoffSnowmeltEnvironmental scienceThunderstormHydrology (agriculture)SnowStormSpring (device)ClimatologyWinter stormGeologyGeographyMeteorology

Abstract

fetched live from OpenAlex

Abstract Many studies have examined trends in the amount and phase of precipitation on the Canadian prairies over the period of record but without considering the unusual hydrology and hydrography of the region. On the Canadian prairies, runoff is primarily due to spring snowmelt over frozen soils but can also be caused by intense rainfall from summer thunderstorms. The fraction of spring snowmelt forming runoff is strongly influenced by the rate of melt and the presence of ice layers near the surface in frozen soils or at the base of the snowpack, all of which can be influenced by rainfall in the spring and late fall. Precipitation intensities sufficient to cause runoff are generally due to small, intense convective storms, which are prevalent during the summer months. Historical records of the fraction of monthly precipitation falling as rain, obtained from the Historical Adjusted Climate Database for Canada (HACDC), were found to display statistically significant increasing trends over the periods 1901–2000 and 1951–2000 at many locations on the Canadian prairies. The fraction of stations showing significant trends, and the importance of the trends, were strongly dependent on the month of the year. Single‐day summer rainfalls are believed to be primarily convective in the Canadian prairies. Historical records obtained from HACDC indicate that the hydrological importance of single‐day summer rainfalls has not increased and has shown significant decreases at many locations over the periods 1901–2000 and 1951–2000. Conversely, the hydrological importance of summer multiple‐day rain events has not decreased and has significantly increased at many locations over the periods analysed. Multiscaling analyses of summer rainfall events demonstrated that the temporal uniformity of rainfall on the Canadian prairies has increased over the periods 1901–2000 and 1951–2000. Analyses of the ratios of rainfall over multiple days demonstrate significant trends over the same periods, confirming the general tendency to temporal uniformity over scales between 1 and 32 days. Longer rain events strongly suggest greater spatial extents for storms and therefore the potential for increasing tendencies to promote basin‐scale rainfall–runoff events such as seen in 2011 in the region. Copyright © 2012 John Wiley & Sons, Ltd.

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)0.001
metaresearch head score (Gemma)0.001
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: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.643
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.001
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)0.0010.000

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 head0.060
GPT teacher head0.235
Teacher spread0.175 · 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