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Record W3041160982

Looking for a relevant potential evapotranspiration model at the watershed scale

2003· preprint· en· W3041160982 on OpenAlexaff
Ludovic Oudin, Frédéric Hervieu, C. Michel, Charles Perrin, François Anctil, Vazken Andréassian

Bibliographic record

VenueHAL (Le Centre pour la Communication Scientifique Directe) · 2003
Typepreprint
Languageen
FieldEnvironmental Science
TopicHydrology and Watershed Management Studies
Canadian institutionsUniversité Laval
Fundersnot available
KeywordsEvapotranspirationWatershedScale (ratio)Environmental scienceComputer scienceHydrology (agriculture)GeologyGeographyCartographyMachine learningEcologyGeotechnical engineering
DOInot available

Abstract

fetched live from OpenAlex

In this paper, we try to identify the most relevant approach to calculate Potential Evapotranspiration (PET) for use in a daily watershed model, to try to bring an answer to the following question : "how can we use commonly available atmospheric parameters to represent the evaporative demand at the catchment scale ?". Hydrologists generally see the Penman model as the ideal model regarding to its good adequacy with lysimeter measurements and its physically-based formulation. However, in real-world engineering situations, where meteorological stations are scarce, hydrologists are often constrained to use other PET formulae with less data requirements or/and long-term average of PET values (the rationale being that PET is an inherently conservative variable). We chose to test 28 commonly used PET models coupled with 4 different daily watershed models. For each test, we compare both PET input options : actual data and long-term average data. The comparison is made in terms of streamflow simulation efficiency, over a large sample of 308 watersheds. The watersheds are located in France, Australia and the United States of America and represent varied climates. Strikingly, we find no systematic improvements of the watershed model efficiencies when using actual PET series instead of long-term averages. This suggests either that watershed models may not conveniently use the climatic information contained in PET values or that formulae are only awkward indicators of the real PET which watershed models need. / Dans ce document, nous avons essayé d'identifier l'approche la plus pertinente pour calculer l'Evapotranspiration Potentielle (ETP) qui serait utilisée dans un model de bassin versant quotidiennement, afin d'essayer de répondre à la question suivante : " Comment pouvons nous utiliser communément des paramètres atmosphériques disponibles pour représenter la demande d'évaporation à l'échelle du basin ? " Nous n'avons pas trouver d'amélioration systématique des efficacités du modèle du bassin versant lorsque nous avons utiliser des séries ETP réelles au lieu de moyennes à long terme. Cela permet de suggérer que les modèles de bassins versants n'utiliseraient pas de façon convenable les informations climatiques contenues dans les valeurs ETP ou que les formules sont seulement des indicateurs maladroits du réel ETP dont les modèles de bassins versants ont besoin.

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)0.001
metaresearch head score (Gemma)0.002
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: none
Teacher disagreement score0.005
Threshold uncertainty score0.011

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.002
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.001
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0010.002
Open science0.0010.000
Research integrity0.0010.001
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 head0.012
GPT teacher head0.212
Teacher spread0.200 · 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 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
Published2003
Admission routes1
Has abstractyes

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