Triple

T21950525
Position Surface form Disambiguated ID Type / Status
Subject Charney–Phillips vertical coordinate E542054 entity
Predicate comparedTo P278 FINISHED
Object Lorenz vertical coordinate NE NERFINISHED

How this triple was built (3 steps)

Every LLM step that produced this triple, in pipeline order — named-entity classification, the disambiguation choices (the exact options shown, with the pick highlighted), and the generated description. The batch + timestamp of each is in the Provenance table below.

NER Named-entity recognition gpt-5-mini
Instruction
Given a phrase, classify it is english named entity (e.g., persons, organizations, works of art) in Latin script, or not (e.g., literals, dates, URLs, verbose phrases). For disambiguation, the statement where the phrase occurs as object is also given. Please return a JSON object with `phrase` (string, the phrase being analyzed) and `is_ne` (boolean, indicating whether the phrase is a Named Entity).
Input
Phrase: Lorenz vertical coordinate | Statement: [Charney–Phillips vertical coordinate, comparedTo, Lorenz vertical coordinate]
NED1 Entity disambiguation (via context triple) gpt-5-mini-2025-08-07
Target entity: Lorenz vertical coordinate
Context triple: [Charney–Phillips vertical coordinate, comparedTo, Lorenz vertical coordinate]
  • A. Charney–Phillips vertical coordinate
    The Charney–Phillips vertical coordinate is a numerical weather prediction grid arrangement that improves the representation of atmospheric stratification and gravity waves by staggering thermodynamic and velocity variables in the vertical.
  • B. Lambert-93
    Lambert-93 is a French national projected coordinate reference system based on the Lambert conformal conic projection, widely used for mapping and geospatial data across mainland France.
  • C. Eady–Eliassen model
    The Eady–Eliassen model is a foundational theoretical framework in atmospheric dynamics used to analyze baroclinic instability and the development of midlatitude weather systems.
  • D. Ertel potential vorticity theorem
    The Ertel potential vorticity theorem is a fundamental result in geophysical fluid dynamics that states potential vorticity is materially conserved for an inviscid, adiabatic flow, making it a key tool for understanding large-scale atmospheric and oceanic motions.
  • E. Lyapunov vector
    A Lyapunov vector is a mathematical construct in dynamical systems theory that characterizes the directions in phase space associated with exponential growth or decay rates quantified by Lyapunov exponents.
  • F. None of above. chosen
  • G. Unsure - the case is ambiguous/there is not enough information to decide.
NED2 Entity disambiguation (via description) gpt-5-mini-2025-08-07
Target entity: Lorenz vertical coordinate
Target entity description: The Lorenz vertical coordinate is a staggered vertical grid arrangement commonly used in atmospheric and numerical weather prediction models, where thermodynamic and mass variables are defined at the same vertical levels.
  • A. Charney–Phillips vertical coordinate chosen
    The Charney–Phillips vertical coordinate is a numerical weather prediction grid arrangement that improves the representation of atmospheric stratification and gravity waves by staggering thermodynamic and velocity variables in the vertical.
  • B. Lambert-93
    Lambert-93 is a French national projected coordinate reference system based on the Lambert conformal conic projection, widely used for mapping and geospatial data across mainland France.
  • C. Eady–Eliassen model
    The Eady–Eliassen model is a foundational theoretical framework in atmospheric dynamics used to analyze baroclinic instability and the development of midlatitude weather systems.
  • D. Ertel potential vorticity theorem
    The Ertel potential vorticity theorem is a fundamental result in geophysical fluid dynamics that states potential vorticity is materially conserved for an inviscid, adiabatic flow, making it a key tool for understanding large-scale atmospheric and oceanic motions.
  • E. Lyapunov vector
    A Lyapunov vector is a mathematical construct in dynamical systems theory that characterizes the directions in phase space associated with exponential growth or decay rates quantified by Lyapunov exponents.
  • F. None of above.

Provenance (2 batches)

The batch behind each pipeline step, in order, with when it ran. Timestamps are batch-level — stages were processed in waves, so the object chain (NER → NED1 → NEDg → NED2) reads in order, but predicate / elicitation batches can sit in a different wave.

Step Stage Batch ID Status When
creating Elicitation batch_69e0c47ef0e48190a50e1bcc43f4b3fd completed April 16, 2026, 11:14 a.m.
NER Named-entity recognition batch_69f1243bb9c88190a3774b9fa2af9871 completed April 28, 2026, 9:18 p.m.
Created at: April 16, 2026, 7:58 p.m.