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Record W3103600114 · doi:10.82308/17783

Use of single Doppler radar observations in data assimilation at convective scale with model as a weak constraint

2010· article· en· W3103600114 on OpenAlexaboutno aff
Kao‐Shen Chung

Bibliographic record

VenueeScholarship@McGill (McGill) · 2010
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicMeteorological Phenomena and Simulations
Canadian institutionsnot available
Fundersnot available
KeywordsDoppler radarDoppler effectData assimilationAssimilation (phonology)RadarScale (ratio)MeteorologyConstraint (computer-aided design)Remote sensingComputer scienceEnvironmental scienceGeologyMathematicsGeographyPhysicsTelecommunications

Abstract

fetched live from OpenAlex

In this work, we have considered several aspects of the McGill radar assimilation system. Currently, information other than radar observations is included in the assimilation system: the forecast of a high-resolution numerical weather prediction model. Besides, the structure of errors of this background term has been improved using a recursive filter. With single-Doppler S-band radar observations, the analyses from the assimilation system proved to successfully generate convection in a rainfall-free background. Furthermore, the system successfully simulated the evolution of a convective storm for more than 30 minutes. To account for the rapid evolution of the convective storms and to correct the forecast errors with time, a cycling process has also been applied. The cycling process helps to maintain the intensity of storm cells for a longer period of time. However, a comparison of radar observations with the 90-min simulation indicated an error in the position of the convective cells. Errors in forecasts, frequently referred to as background errors, result from errors in the initial conditions that grow through non-linear model equations with imperfect physical parameterizations. However, estimating forecast errors is not straightforward since the true atmospheric state is never exactly known. Ensemble forecasting is a feasible way to characterize the structure of forecasting errors and represent the probability distribution of plausible atmospheric states. In our work, an ensemble scheme has been applied to understand the structure of background errors at convective scale. The analysis has consisted in perturbing radar observations with two sets of simulated errors: one that neglects the spatial correlation of radar errors, and another where their spatial correlation is prescribed. The sensitivity of the system to such perturbations has been studied over a convective case. The results demonstrated that neglecting the correlation of radar errors badly limits the spread of ensembles and underestimates the model error correlation. In addition, further studies on the cross-correlations between different control variables illustrated the strong connection between the dynamics and the microphysical processes as depicted by the model. Our work also included the analysis of the different features of the background error within and outside the precipitation regions.

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)0.001
metaresearch head score (Gemma)0.002
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: none
Teacher disagreement score0.016
Threshold uncertainty score0.032

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.002
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0010.001
Open science0.0010.001
Research integrity0.0010.001
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 head0.102
GPT teacher head0.243
Teacher spread0.141 · 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
Published2010
Admission routes1
Has abstractyes

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