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Kosñipata River discharge at San Pedro and Wayqecha, Peru (Clark et al. 2014)

2017· dataset· en· W4236604886 on OpenAlexfundno aff
Kathryn E. Clark, Mark A. Torres, Josh West, Robert Hilton, Mark New, Aline B. Horwath, Joshua A. Fisher, Joshua M. Rapp, A Robles Caceres, Yadvinder Malhi

Bibliographic record

VenueHydroShare Resources · 2017
Typedataset
Languageen
FieldEnvironmental Science
TopicEnvironmental and Cultural Studies in Latin America and Beyond
Canadian institutionsnot available
FundersClarendon FundHORIZON EUROPE European Research CouncilNatural Sciences and Engineering Research Council of CanadaJackson FoundationNational Science Foundation
KeywordsArchaeologyGeographyArt

Abstract

fetched live from OpenAlex

Please cite: Clark, K. E., Torres, M. A., West, A. J., Hilton, R. G., New, M., Horwath, A. B., Fisher, J. B., Rapp, J. M., Robles Caceres, A., and Malhi, Y. (2014), The hydrological regime of a forested tropical Andean catchment, Hydrology and Earth System Sciences, 18, 5377-5397, doi: 10.5194/hess-18-5377-2014. Sheet 1: Discharge measurements at the San Pedro gauging station (1360 m.a.s.l.), along the Kosñipata River, in the Andes of Peru. The Kosñipata River at the San Pedro gauging station drains an area of 164.4 km2. Field measurements consisted of river height, flow velocity, and cross-sectional area, which together allowed us to estimate discharge and runoff over the study period. River stage height was measured from January 2010 to February 2011 using a river logger (GlobalWater WL16 Data Logger, range 0–9 m), recording river level every 15 min. The instantaneous discharge associated with each height measurement was calculated based on calibrated stage–discharge relationships. The Kosñipata River discharge at San Pedro was measured through a complete water year, with a 31-day gap partly in July and August (during low flow) that was covered by three manual measurements and the gap was filled using linear interpolation. Sheet 2: Weekly to monthly discharge measurements at the Wayqecha gauging station (2250 m.a.s.l), along the Kosñipata River, in the Andes of Peru. The Wayqecha sub-catchment a nested catchment upstream of the San Pedro gauging station. It encompasses the headwaters of the Kosñipata River, draining an area of 48.5 km2 (See the supplementary information in Clark et al. 2014). Locations of the San Pedro and Wayqecha gauging stations are provided as GIS coverages in a companion dataset. This product was created by Kathryn Clark (kathryn.clark23@gmail.com). Other related datasets from Clark et al. (2014): Clark, K., J. West, R. Hilton (2017). Andes-Amazon gauging stations (Clark et al. 2014), HydroShare, http://www.hydroshare.org/resource/b541f44606a44a4a911e0e09d1b88d74 Clark, K., J. West, R. Hilton (2017). Kosñipata River at San Pedro, Peru (Clark et al. 2014), HydroShare, http://www.hydroshare.org/resource/b54b1cc138c54004a669f91a5351166e Clark, K., J. West, R. Hilton (2017). Catchment boundary, Kosñipata River at San Pedro, Peru (Clark et al. 2014), HydroShare, http://www.hydroshare.org/resource/0677a428cbd64d0ab62f7ab7a8e112f3 Clark, K., J. West, R. Hilton (2017). Catchment boundary, Kosñipata River at Wayqecha, Peru (Clark et al. 2014), HydroShare, http://www.hydroshare.org/resource/8a21d07106564bcdb2d183c77a5de877

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)0.003
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Dataset · Consensus signal: Dataset
Teacher disagreement score0.112
Threshold uncertainty score0.222

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.003
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0030.006
Science and technology studies0.0000.000
Scholarly communication0.0010.001
Open science0.0020.001
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0120.010

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 head0.011
GPT teacher head0.256
Teacher spread0.245 · 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 designNot applicable
Domainnot available
GenreDataset

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
Published2017
Admission routes1
Has abstractno

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