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Review of rainfall frequency estimation methods

2010· article· en· W2137354438 on OpenAlex
Cecilia Svensson, D. A. Jones

Why this work is in the frame

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aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueJournal of Flood Risk Management · 2010
Typearticle
Languageen
FieldEnvironmental Science
TopicHydrology and Drought Analysis
Canadian institutionsnot available
Fundersnot available
KeywordsRegionalisationEstimationFlood mythReturn periodGeographyDistribution (mathematics)Environmental sciencePhysical geographyStatisticsEconometricsClimatologyMathematicsGeologyEconomic geographyEconomics

Abstract

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Abstract This review outlines nationwide methods for point rainfall frequency estimation currently in use in nine different countries: Canada, Sweden, France, Germany, the United States, South Africa, New Zealand, Australia and the United Kingdom. For the United Kingdom, the Flood Studies Report method from 1975 is described as well as the current Flood Estimation Handbook method. The focus is on return periods relevant to reservoir design, in the region of 100–10 000 years. There is considerable difficulty in estimating long return period rainfalls from short data records and there is no obviously ‘best’ way of doing it. Each country's method is different, but most use some form of regionalisation to transfer information from surrounding sites to the target point. Several of the methods are variations of a regionalisation method that combines a local estimate of an index variable (typically the mean or the median annual maximum rainfall) with a regionally derived growth curve to obtain a design rainfall estimate. Three of the methods use regions centred on the site of interest, rather than fixed‐boundary regions. Different statistical distributions and fitting methods are used, with the Generalised Extreme Value distribution being the most common.

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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)0.003
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: Other design · Consensus signal: none
GenreCandidate signal: Methods · Consensus signal: Methods
Teacher disagreement score0.916
Threshold uncertainty score0.998

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0030.000
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 head0.007
GPT teacher head0.298
Teacher spread0.292 · 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