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A spatial and temporal stochastic cascade analysis of meteorological models and reanalyses

2009· dissertation· en· 0 citations· W7033856201 on OpenAlex

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A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

Canadian funderA Canadian agency funded it. The work may carry no Canadian affiliation at all.

No Canadian affiliation. An affiliation-only frame — the usual design — would never have seen this work. It is one of the works that make the case for inverting the frame.

The three-model screen

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All three models called this out of scope.

stratum: fund_new · design weight: 1678.90 (the sample is stratified; any rate computed without the weight is wrong)
Claude Opus 4.8OUT
genre: empirical
about Canada: no
confidence: medium

Atmospheric science thesis on cascade structure of weather models and reanalyses; what we learn is about the atmosphere, not about research practice.

GPT-5.6 (high)OUT
genre: empirical
about Canada: no
confidence: high

The thesis studies stochastic structures in atmospheric models and reanalyses, not research methodology.

Grok 4.5OUT
genre: empirical
about Canada: no
confidence: high

Stochastic cascade analysis of weather models and reanalyses; atmospheric science, not study of research methods.

Abstract

This thesis investigates the hypothesis that the stochastic structure of deterministic models of the atmosphere is captured by multiplicative cascade processes. Using data from reanalyses (ERA 40) and two meteorological models (GFS, GEM), we investigate the spatial and temporal cascade structures of the temperature, humidity, and horizontal wind at various altitudes, latitudes, and forecast times. Over the range spanning from the model dissipation scales (≈100 km) to at least 5000 km and for statistical moments up to order 2, the cascade predictions are satisfied to typically better than ±1%. In time, we find corresponding cascade structures with outer scales of roughly 15 days. By constructing space-time diagrammes, we find they are roughly linear up to 5-10 days with transformation velocities of about 1000 km/day, as predicted based on the solar energy flux. This transition time scale, which corresponds to planetary size structures, objectively defines the weather/climate transition.

Stored with the screening record, where it is evidence for the labels above.

The record

Venue
eScholarship@McGill (McGill)
Topic
Educational Reforms and Innovations
Field
Environmental Science
Canadian institutions
Funders
Natural Sciences and Engineering Research Council of Canada
Keywords
CascadeMultiplicative functionRange (aeronautics)Stochastic modellingTransformation (genetics)DissipationStochastic process
Has abstract in OpenAlex
yes