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Record W2400342579 · doi:10.14288/1.0096022

Effects of forest harvesting on snowmelt during rainfall in coastal British Columbia

2010· article· en· W2400342579 on OpenAlexaboutno aff
P. G. Beaudry

Bibliographic record

VenuecIRcle (University of British Columbia) · 2010
Typearticle
Languageen
FieldEnvironmental Science
TopicLandslides and related hazards
Canadian institutionsnot available
Fundersnot available
KeywordsSnowmeltEnvironmental scienceHydrology (agriculture)ForestrySnowPhysical geographyGeographyMeteorologyGeology

Abstract

fetched live from OpenAlex

Rain-on-snow has been recognized as an event with potential for increasing flood and debris torrent hazards. However the effects of deforestation on increasing this hazard are not well understood. To better understand this phenomena a study was conducted in the Jamieson Creek experimental watershed near Vancouver B.C. Its primary objective was to determine the effects of forest harvesting on snow melt rates and subsequent runoff during rain-on-snow events. The energy balance of a snowcover and the theory of snowmelt are reviewed to better understand the processes involved during rain-on-snow. Techniques and instrumentation required to compute the energy budget are discussed, with the aerodynamic technique receiving greater attention. Also reviewed are the U.S. Army Corps of Engineers (1956) snowmelt equations and their applicability for rain-on-snow situations. The experimental set-up consisted of two study plots, one located in a recent cutover and a second in an adjacent Coastal Western Hemlock old-growth forest. Each plot was equipped with a large (22m[sup 2]) plastic sheet lysimeter recording through a tipping bucket arrangement, allowing comparison of snowmelt and runoff rates between sites. Direct measurement of snowmelt was also achieved using snow survey techniques. The USACE(1956) snowmelt equations were verified by comparing the computed melt with the lysimeter and snow survey results. Wind speed, relative humidity and air temperatures were measured at 0.6 and 1.5 meters above the snowpack to evaluate latent and sensible heat fluxes. Snowpack and ground heat exchanges were measured with a profile of five thermistors, and radiation was monitored with net all-wave radiometers. Three winters of data were collected (1981-82, 1982-83, 1983-84), with several storms being analysed from each of the last two years. Peak runoff intensities and total runoff amounts, during rain-on-snow were found to be greater at the forest site when there was presence of snow in the canopy. When there was no snow in the canopy runoff was always greater at the open site. The reasons for the greater runoff at either of the sites are discussed. The use of the USACE (1956) snowmelt equations generally compared favorably with the snow survey and lysimeter data, at the open site. However under certain specific conditions these snowmelt equations were shown to be inadequate for use at the forest site. The role of the forest canopy on snow and rainfall interception played a major role in explaining the differences in snowmelt and runoff rates encountered between the two sites.

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)0.001
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 score0.146
Threshold uncertainty score0.295

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.003
GPT teacher head0.147
Teacher spread0.145 · 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

Citations6
Published2010
Admission routes1
Has abstractyes

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