MétaCan
Menu
Back to cohort
Record W2885975814 · doi:10.82308/32233

Thermally-driven circulation and convection over a mountainous tropical island

2014· article· en· W2885975814 on OpenAlexaff
Chun‐Chih Wang

Bibliographic record

VenueeScholarship@McGill (McGill) · 2014
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicMeteorological Phenomena and Simulations
Canadian institutionsMcGill University
Fundersnot available
KeywordsCirculation (fluid dynamics)ClimatologyConvectionTropicsGeographyGeologyMeteorologyEnvironmental scienceMechanicsPhysics

Abstract

fetched live from OpenAlex

Observational data from the 2011 Dominica Experiment (DOMEX) and cloud-resolving numerical simulations are exploited in order to acquire a better understanding of controlling parameters of thermally-driven circulation and convection over a mountainous tropical island. Four weak (<4 m/s) background wind days are investigated to obtain a preliminary diagnosis of the conditions favorable for diurnally-forced shallow cumulus convection over the island. The observations suggest that the degree of solar heating before the first cumulus development largely controls the amount of low-level forcing and the vigor of shallow cumulus, rather than the moist stability of the background flow.A “golden” case from DOMEX with a clear diurnal cycle in cumulus convection is studied using quasi-idealized numerical simulations (with full model physics and a realistic terrain profile) to better understand the mechanisms and sensitivities of island thermal circulations and cumulus convection. Simulations at different grid spacings reveal that large-eddy grid spacing (~100 m) provides the most accurate representation of the in-situ measurements from DOMEX and other observations. Sensitivity tests reveal that mechanical forcing played little role in convection initiation on this day since the Froude number (Fr) was < 1. Surprisingly, even though thermal circulations develop earlier over a mountainous island, they are ultimately weaker than those over a flat island possibly due to their elevated outflows undergo stable descent over a high terrain. Background wind velocity also has a significant impact on thermal circulations, which tend to weaken as the cross-barrier wind increases. Cloud shadowing and precipitation both have a negative feedback on thermal circulations, with the former being the stronger mechanism. In addition, cloud latent-heat release over the island strengthens thermal circulations, which also explains why circulations intensify when cumulus vigor is enhanced by greater moist instability.The simulations allow for the evaluation of thermal-circulation-strength predictions from thermodynamic heat engine theory. While the theory predicts the strength of thermal circulations reasonably well over a mountainous terrain, it fails to capture the sensitivity to terrain height likely because its assumption that the entire circulation is confined within the mixed layer is invalid.

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: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.081
Threshold uncertainty score0.160

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 head0.208
Teacher spread0.192 · 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

Citations2
Published2014
Admission routes1
Has abstractyes

Explore more

Same venueeScholarship@McGill (McGill)Same topicMeteorological Phenomena and SimulationsFrench-language works237,207