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Record W7027046991

Changing Snowmelt Conditions in the Western Canadian Arctic

2022· article· en· W7027046991 on OpenAlexaboutno aff

Bibliographic record

VenueScholars Commons (Wilfrid Laurier University) · 2022
Typearticle
Languageen
FieldArts and Humanities
TopicHistorical Studies on Reproduction, Gender, Health, and Societal Changes
Canadian institutionsnot available
Fundersnot available
KeywordsSnowmeltArcticSubpoenaSnowTingling
DOInot available

Abstract

fetched live from OpenAlex

Multidecadal Changes in Spring Snowmelt in the Western Canadian Arctic\nThis study investigates the changes in key aspects of snowmelt in the western Canadian Arctic. Specifically, we will look at changes in the onset of snowmelt and the duration of snowmelt between 1999 and 2019, and extended air temperature between 1957 and 2019. In addition, we will look at changes in eight meteorological variables during the melt period. It was found that the onset of snowmelt occurred 14 days earlier, while the melt period ends 20 days earlier than 20 years ago. As a result, the duration of melt period has decreased by 5 days. During this earlier and shorter melt period, the air temperature and relative humidity have both increased. While these changes were statistically significant, there were no statistically significant changes in SWE, precipitation, wind speed, downward shortwave and longwave radiation, or refreeze events. Future research will consider the effects and the variability of these changes on the snowmelt energy balance.\nChanging Snowmelt Energy Balance in the Western Canadian Arctic\nThe hydrology of the of the Arctic is dominated by the accumulation of snow over the long winter, and the rapid melt of this snow over a few weeks in the spring. This aspect of the Arctic water cycle is especially sensitive to a warming climate. The timing and the rate of snow melt during the spring period has implications for aquatic ecosystems and communities that depend on melt water. As shown in Chapter 2, the western Canadian Arctic has experienced an earlier onset of snowmelt compared to earlier decades, a warmer and shorter melt period. The changes in the energy balance components are tied to climate warming, and therefore, controlling the rate of snowmelt. In this paper we will use a physically based snowmelt model to investigate changes in the energy transfers between the snow surface and the atmosphere during the snowmelt period over the last 21 years. Model runs demonstrate that radiation plays a decisive role, followed by turbulent fluxes of sensible heat and latent heat. A shorter duration of melt is due to a combination of changes in the end of winter SWE and meteorological conditions. As net radiation and warmer air temperatures increased, we found an increase to the rate of snowmelt by 0.7 mm/day per decade.

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 score0.022
Threshold uncertainty score0.159

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.004
Science and technology studies0.0030.000
Scholarly communication0.0010.000
Open science0.0010.001
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 head0.042
GPT teacher head0.228
Teacher spread0.186 · 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

Citations0
Published2022
Admission routes1
Has abstractyes

Explore more

Same venueScholars Commons (Wilfrid Laurier University)→Same topicHistorical Studies on Reproduction, Gender, Health, and Societal Changes→French-language works237,207→