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Record W3191079559

Assessing trends in temperature, precipitation and streamflow due to climate change in Credit River watershed

2009· article· en· W3191079559 on OpenAlexaboutno aff
Ajai Singh, J. W. Dougherty, Christine Zimmer, J. Kinkead, Mike Hulley, Conor Doherty

Bibliographic record

VenueOSTI OAI (U.S. Department of Energy Office of Scientific and Technical Information) · 2009
Typearticle
Languageen
FieldEnvironmental Science
TopicHydrology and Watershed Management Studies
Canadian institutionsnot available
Fundersnot available
KeywordsStreamflowClimate changePrecipitationEnvironmental scienceWatershedGlobal warmingClimatologyWater cycleWater resourcesGreenhouse gasEffects of global warmingGeographyDrainage basinEcologyMeteorologyGeology
DOInot available

Abstract

fetched live from OpenAlex

'Full text:' Studies on climate change at Natural Resources Canada showed that average temperature in Canada increased by 0.9°C since 1948 and further estimated that Ontario will warm by an average of 2°C to 5°C within the next 75 to 100 years. The climate change is linked to the anthropogenic activities which are understood to increasing green house gasses concentrations in the Earth's atmosphere thereby warming the planet. The warming is further related to affecting the components of hydrological cycle such as precipitation intensities, durations, snowfall, streamflow peaks, low flows etc. According to the Intergovernmental Panel on Climate Change (IPCC) Technical Paper on Climate Change and Water “Observational records and climate projections provide abundant evidence that freshwater resources are vulnerable and have the potential to be strongly impacted by climate change, with wide-ranging consequences for human societies and ecosystems.” The Ministry of Natural Resources projected temperature and precipitation changes for Southern Ontario for period 2075-2100 indicate 3-5°C higher summer and 5-6°C higher winter temperatures and ±10% change in annual precipitation from 1971-2000 using higher green house gas emission scenario (A2). However, the changes in climate and their effect on hydrological cycle could differ locally and these effects could be assessed using local historical data. Therefore, the Valley Conservation Authority initiated a study to assess how the climate change has affected the Credit River watershed by investigating trends in the historical temperature, precipitation and streamflow data sets. The temperature trends were analysed for mean, maximum and minimum temperatures on annual and monthly basis from nine meteorological stations located within or close to the Credit River watershed. The precipitation data from the same nine meteorological stations were used to analyse a) Intensity-Duration-Frequency (IDF) patterns of 1, 2, 6, 12 and 24 hr rainfall duration and 2, 5, 10, 50 year recurrence intervals; b) extreme annual precipitation for 1, 2, 6, 12 and 24 hr duration; and c) mean monthly and seasonal precipitation. The streamflow trend analysis was conducted at nine locations across the Credit River watershed on monthly, seasonal and annual basis. The visual interpretation of the time series plotting and statistical testing of the data for identifying trends has been completed for the study and the results from the analysis are being investigated. (author)

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)0.000
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: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.644
Threshold uncertainty score0.708

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.002
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.003
Science and technology studies0.0000.000
Scholarly communication0.0010.000
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 head0.013
GPT teacher head0.246
Teacher spread0.232 · 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 designObservational
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

Citations1
Published2009
Admission routes1
Has abstractyes

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