MétaCan
Menu
← Back to cohort
Record W4413246345 · doi:10.5194/ecss2025-123

Synoptic Analysis and Simulation of the High-Shear, Low-CAPE (HSLC) F4-Tornado in Hautmont, France from August 03, 2008 using ERA5 data and Cloud Model

2025· article· en· W4413246345 on OpenAlexaff
Oliver Heuser, Lisa Schielicke, Petra Friederichs

Bibliographic record

Venuenot available
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicMeteorological Phenomena and Simulations
Canadian institutionsWestern University
Fundersnot available
KeywordsTornadoMesocycloneMeteorologyThunderstormGeologyConvectionEnvironmental scienceStormClimatologySevere weatherJet (fluid)CyclogenesisSupercellBoundary layerAtmospheric sciencesGeographyMechanicsComputer scienceCyclone (programming language)EngineeringAerospace engineeringPhysicsDoppler radarRadar

Abstract

fetched live from OpenAlex

On August 03, 2008, an F4 tornado struck the city of Hautmont, France, causing extensive damage across seven municipalities and injuring numerous individuals during its 14-minute lifespan. The tornado developed from a pre-frontal convective system within a high-shear, low-CAPE (HSLC) environment - a setting in which the occurrence of strong tornadoes is considered atypical. This study aims to analyze the synoptic-scale situation with a particular focus on tornado-favorable and convectively relevant parameters, utilizing ERA5 reanalysis data. A reconstructed atmospheric sounding and hodograph were used as initial conditions for idealized simulations with the Cloud Model 1 (CM1), incorporating various convective initiation triggers. The objective was to explore potential polarimetric signatures indicative of supercellular structures or bow echoes.The analysis indicates that a jet coupling event triggered quasi-geostrophic cyclogenesis, which led to the development of a surface low and the formation of a low-level jet. Together with high moisture content near the surface and within the atmospheric boundary layer, these factors were identified as key contributors to tornadogenesis in this case.Simulation results highlight limitations in representing soundings with high boundary layer moisture within CM1. Among the tested initiation triggers, updraft nudging proved to be the most effective and, in fact, the only one capable of producing a tornado-like vortex. This suggests that updraft nudging can enhance or even partially compensate for the inherently weak convective updrafts in HSLC environments, potentially enabling the formation of short-lived supercells following convection initiation. Based on these findings, it is proposed to conceptually differentiate between two categories of convective triggers: those that initiate convection and those that support and maintain it under marginal conditions.As an outlook first attempts of creating a series of synthetic idealizied soundings for the use of numerical simulations were attemptend with the goal of testing the limits and boundaries of various numerical convective simulation models.

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: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.127
Threshold uncertainty score0.253

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0000.001
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0010.000
Open science0.0010.000
Research integrity0.0010.001
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 head0.031
GPT teacher head0.253
Teacher spread0.222 · 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
Published2025
Admission routes1
Has abstractyes

Explore more

Same topicMeteorological Phenomena and Simulations→French-language works237,207→