MétaCan
Menu
← Back to cohort
Record W2884584638 · doi:10.82308/49908

Synoptic control over orographic precipitation distributions during OLYMPEX

2017· article· en· W2884584638 on OpenAlexaff
David Purnell

Bibliographic record

VenueeScholarship@McGill (McGill) · 2017
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicMeteorological Phenomena and Simulations
Canadian institutionsMcGill University
Fundersnot available
KeywordsPrecipitationOrographyClimatologyOrographic liftEnvironmental scienceMeteorologyAtmospheric sciencesGeographyGeology

Abstract

fetched live from OpenAlex

During the Olympic Mountains Experiment (OLYMPEX) in Washington State in winter 2015-16, intensive precipitation and upper-air measurements were obtained within frontal systems traversing the Olympic mountain range. In this study, an analysis and interpretation of the observed precipitation distributions, as a function of synoptic conditions, is undertaken. The synoptic conditions are categorized as warm-frontal (ahead of a surface warm front), warm-sector (between the surface warm and cold fronts), and post-frontal (behind the surface cold front). Six periods of each frontal class are selected, for which observed precipitation distributions are retrieved using a combination of operational S-band radars and a relatively dense regional rain-gauge network. Radar and rain gauge data is merged using a unique combination of bias correction and optimal estimation techniques. Not surprisingly, far greater orographic precipitation amounts are observed during warm-frontal and warm-sector periods than during post-frontal periods. The warm-sector periods exhibit the largest orographic enhancement directly over the massif, the warm-frontal periods exhibit a smaller enhancement over a large area upstream of the mountain and the post-frontal periods are characterised by a local maximum at the foot of the mountain. Analysis of upstream soundings indicates that the upstream shift of precipitation in warm frontal and postfrontal conditions is associated with a large nondimensional mountain height, suggesting strong upstream blocking. To enhance the physical interpretation, quasi-idealized simulations with the Weather Research and Forecasting (WRF) model are conducted. The simulations use the real Olympics terrain and idealized soundings based on the upper-air observations. Crucially, upstream precipitation (an element often missing from idealized orographic precipitation simulations) is considered by applying a large-scale lifting profile in the warm-frontal and warm-sector simulations, or by producing oceanic cellular convection upstream of the Olympics for the post-frontal simulations. Key differences between observed frontal periods are reproduced by the simulations. Sensitivity tests of upstream precipitation indicate that while the structure of the orographic enhancement fundamentally changes when upstream precipitation is included, the degree of orographic enhancement is not strongly dependent on the intensity of the upstream precipitation.

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: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.019
Threshold uncertainty score0.039

Distilled classifier scores by category (both heads)

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

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 head0.018
GPT teacher head0.226
Teacher spread0.208 · 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 designSimulation or modeling
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
Published2017
Admission routes1
Has abstractyes

Explore more

Same venueeScholarship@McGill (McGill)→Same topicMeteorological Phenomena and Simulations→French-language works237,207→