Triple
T21172736
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Ertel potential vorticity theorem |
E521730
|
entity |
| Predicate | concernsQuantity |
P79687
|
FINISHED |
| Object | Ertel potential vorticity |
—
|
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: Ertel potential vorticity | Statement: [Ertel potential vorticity theorem, concernsQuantity, Ertel potential vorticity]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Ertel potential vorticity Context triple: [Ertel potential vorticity theorem, concernsQuantity, Ertel potential vorticity]
-
A.
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.
-
B.
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.
-
C.
Charney–Eliassen model
The Charney–Eliassen model is a foundational quasi-geostrophic framework in atmospheric dynamics used to describe large-scale, balanced motions such as midlatitude cyclones and jet streams.
-
D.
Bjerknes circulation theorem (applications in meteorology)
The Bjerknes circulation theorem is a fundamental principle in meteorology that relates changes in atmospheric circulation to forces such as pressure gradients and heating, forming a basis for understanding large-scale weather systems and cyclogenesis.
-
E.
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.
- 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: Ertel potential vorticity Target entity description: Ertel potential vorticity is a conserved dynamical quantity in geophysical fluid dynamics that combines fluid vorticity, stratification, and rotation to describe the evolution of rotating, stratified flows such as the atmosphere and oceans.
-
A.
Ertel potential vorticity theorem
chosen
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.
-
B.
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.
-
C.
Charney–Eliassen model
The Charney–Eliassen model is a foundational quasi-geostrophic framework in atmospheric dynamics used to describe large-scale, balanced motions such as midlatitude cyclones and jet streams.
-
D.
Bjerknes circulation theorem (applications in meteorology)
The Bjerknes circulation theorem is a fundamental principle in meteorology that relates changes in atmospheric circulation to forces such as pressure gradients and heating, forming a basis for understanding large-scale weather systems and cyclogenesis.
-
E.
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.
- 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_69e0b50e30748190b186824a206d39b9 |
completed | April 16, 2026, 10:08 a.m. |
| NER | Named-entity recognition | batch_69e727141b7c81908eb8ca92850736a4 |
completed | April 21, 2026, 7:28 a.m. |
Created at: April 16, 2026, 3 p.m.