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Record W2076711862 · doi:10.1029/2007jg000653

Water flux components and soil water‐atmospheric controls in a temperate pine forest growing in a well‐drained sandy soil

2008· article· en· W2076711862 on OpenAlexaffabout
Joshua McLaren, M. Altaf Arain, Myroslava Khomik, Matthias Peichl, Jason Brodeur

Bibliographic record

VenueJournal of Geophysical Research Atmospheres · 2008
Typearticle
Languageen
FieldEnvironmental Science
TopicPlant Water Relations and Carbon Dynamics
Canadian institutionsMcMaster University
Fundersnot available
KeywordsVapour Pressure DeficitTranspirationEddy covarianceEnvironmental scienceCanopyAtmospheric sciencesSoil waterHydrology (agriculture)UnderstoryTemperate forestGrowing seasonEvapotranspirationFlux (metallurgy)Context (archaeology)Temperate climateSoil scienceEcosystemEcologyGeographyChemistryGeology

Abstract

fetched live from OpenAlex

The influences of soil water supply and atmospheric demand on transpiration were studied to gain insight into the physical mechanisms limiting forest water use within the broader context of total canopy water loss to the atmosphere. Evaporation from forests (E) can be partitioned in to four main source components: canopy transpiration (Ec), understorey transpiration (Eu), evaporation from the soil (Es), and the evaporation of intercepted water (EI). Ec and EI usually make up most of E. Ec estimated from sap flow measurements and modeled EI estimates were compared with eddy covariance measured values of E to quantify the components of the above canopy water flux to the atmosphere, in a temperate pine forest ecosystem established on a well‐drained sandy plain at Turkey Point in southern Ontario, Canada. Daily values of E averaged 2.4 mm d−1 and reached maximums of 4 mm d−1 while daily values of Ec averaged 1.2 mm d−1 over the growing season. The evaporation of intercepted water (EI) was generally between 2 and 3 mm per event. EI accounted for 34% and Ec accounted for 47% (31 to 67% range on a monthly basis), together accounting for 81% of E during the growing season. Ec increased linearly with vapor pressure deficit (VPD) until a transition point was reached, after which mid‐day Ec rates remained more or less constant. For analysis purposes, data were segregated by early morning VPD (or VPDin) in an attempt to characterize the atmosphere at the beginning of the daily transpiration cycle. This technique revealed that shifts in the timing and magnitude of Ec rates masked the response of Ec to changes in soil water content. Analysis also suggested that while increasing VPDs may limit maximum transpiration rates, daily total transpiration is a conservative quantity. This study improves the understanding of the physical mechanisms limiting water loss in forested ecosystems growing on water‐stressed soils by investigating the effects of VPD and soil water content on Ec.

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)0.000
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 score0.138
Threshold uncertainty score0.275

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
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)0.0000.000

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 head0.016
GPT teacher head0.248
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

Citations38
Published2008
Admission routes2
Has abstractyes

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