Triple
T15145206
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Indian Ocean Dipole |
E361786
|
entity |
| Predicate | relatedTo |
P37
|
FINISHED |
| Object |
Indian Ocean Basin Mode
The Indian Ocean Basin Mode is a large-scale pattern of sea surface temperature variability across the entire tropical Indian Ocean that influences regional climate and monsoon systems.
|
E361786
|
NE FINISHED |
How this triple was built (4 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: Indian Ocean Basin Mode | Statement: [Indian Ocean Dipole, relatedTo, Indian Ocean Basin Mode]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Indian Ocean Basin Mode Context triple: [Indian Ocean Dipole, relatedTo, Indian Ocean Basin Mode]
-
A.
Indian Ocean circulation
Indian Ocean circulation refers to the large-scale system of currents, gyres, and seasonal monsoon-driven flows that redistribute heat, salt, and nutrients throughout the Indian Ocean basin.
-
B.
Indian Ocean Dipole
The Indian Ocean Dipole is a climate phenomenon characterized by irregular sea surface temperature differences between the western and eastern Indian Ocean, which strongly affects regional weather patterns such as rainfall and monsoon behavior.
-
C.
Atlantic Meridional Mode
The Atlantic Meridional Mode is a pattern of sea surface temperature variability in the tropical Atlantic that influences regional climate, including rainfall and wind patterns.
-
D.
Atlantic Niño variability
Atlantic Niño variability refers to the irregular warming and cooling of sea surface temperatures in the eastern equatorial Atlantic that strongly influences regional climate and rainfall patterns in surrounding continents.
-
E.
Indian Ocean subtropical gyre
The Indian Ocean subtropical gyre is a large, clockwise-rotating system of ocean currents in the southern Indian Ocean that plays a key role in heat transport, climate regulation, and marine ecosystems.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
NEDg
Description generation
gpt-5.1
Instruction
Generate a one-sentence description of the target entity. You are given a context triple in the form (subject, predicate, object), where the object is the target entity. # Instructions Use the triple to infer relevant information about the entity. Describe the entity based on what is most defining, well-known. Avoid repeating the information from the triple, unless really essential. # Response Format Return only the sentence: "Description: [one-sentence description of the target entity]"
Input
Entity: Indian Ocean Basin Mode Triple: [Indian Ocean Dipole, relatedTo, Indian Ocean Basin Mode]
Generated description
The Indian Ocean Basin Mode is a large-scale pattern of sea surface temperature variability across the entire tropical Indian Ocean that influences regional climate and monsoon systems.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Indian Ocean Basin Mode Target entity description: The Indian Ocean Basin Mode is a large-scale pattern of sea surface temperature variability across the entire tropical Indian Ocean that influences regional climate and monsoon systems.
-
A.
Indian Ocean circulation
Indian Ocean circulation refers to the large-scale system of currents, gyres, and seasonal monsoon-driven flows that redistribute heat, salt, and nutrients throughout the Indian Ocean basin.
-
B.
Indian Ocean Dipole
chosen
The Indian Ocean Dipole is a climate phenomenon characterized by irregular sea surface temperature differences between the western and eastern Indian Ocean, which strongly affects regional weather patterns such as rainfall and monsoon behavior.
-
C.
Atlantic Meridional Mode
The Atlantic Meridional Mode is a pattern of sea surface temperature variability in the tropical Atlantic that influences regional climate, including rainfall and wind patterns.
-
D.
Atlantic Niño variability
Atlantic Niño variability refers to the irregular warming and cooling of sea surface temperatures in the eastern equatorial Atlantic that strongly influences regional climate and rainfall patterns in surrounding continents.
-
E.
Indian Ocean subtropical gyre
The Indian Ocean subtropical gyre is a large, clockwise-rotating system of ocean currents in the southern Indian Ocean that plays a key role in heat transport, climate regulation, and marine ecosystems.
- F. None of above.
Provenance (5 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_69d85a0759908190b8a051d2e2a1cbe6 |
completed | April 10, 2026, 2:01 a.m. |
| NER | Named-entity recognition | batch_69e005c71b688190b2e8ccfdf4db9037 |
completed | April 15, 2026, 9:40 p.m. |
| NED1 | Entity disambiguation (via context triple) | batch_69febff02e648190bd10f04a374da227 |
completed | May 9, 2026, 5:02 a.m. |
| NEDg | Description generation | batch_69fec08c37dc8190a59289e4ee76beab |
completed | May 9, 2026, 5:05 a.m. |
| NED2 | Entity disambiguation (via description) | batch_69fec10cd2d48190ba96885ca604a853 |
completed | May 9, 2026, 5:07 a.m. |
Created at: April 10, 2026, 3:07 a.m.