Triple
T584891
| Position | Surface form | Disambiguated ID | Type / Status |
|---|---|---|---|
| Subject | Arabian Sea |
E15136
|
entity |
| Predicate | climateInfluencedBy |
P9
|
FINISHED |
| Object |
Northeast monsoon
The Northeast monsoon is a seasonal wind and rainfall pattern that brings cooler, dry or sometimes heavy rain-bearing air from the Asian continent toward the Indian Ocean, significantly affecting weather in South and Southeast Asia.
|
E73568
|
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: Northeast monsoon | Statement: [Arabian Sea, climateInfluencedBy, Northeast monsoon]
NED1
Entity disambiguation (via context triple)
gpt-5-mini-2025-08-07
Target entity: Northeast monsoon Context triple: [Arabian Sea, climateInfluencedBy, Northeast monsoon]
-
A.
Southwest monsoon
The Southwest monsoon is a seasonal wind and rainfall system that brings warm, moisture-laden air from the Indian Ocean and Arabian Sea to South Asia, producing the region’s primary rainy season.
-
B.
Indian Monsoon Current
The Indian Monsoon Current is a seasonally reversing ocean current in the northern Indian Ocean driven by the South Asian monsoon winds, significantly influencing regional climate and marine circulation.
-
C.
Madden–Julian Oscillation
The Madden–Julian Oscillation is a large-scale tropical atmospheric pattern characterized by eastward-moving pulses of enhanced and suppressed rainfall that strongly influence global weather and climate variability on intraseasonal timescales.
-
D.
La Niña
La Niña is the cool phase of the El Niño–Southern Oscillation climate pattern, characterized by unusually cold ocean temperatures in the central and eastern equatorial Pacific and associated shifts in global weather.
-
E.
Bora wind
The Bora wind is a cold, dry, and often violent northeasterly wind that blows from the interior highlands toward the Adriatic Sea, especially affecting coastal areas like Trieste.
- 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: Northeast monsoon Triple: [Arabian Sea, climateInfluencedBy, Northeast monsoon]
Generated description
The Northeast monsoon is a seasonal wind and rainfall pattern that brings cooler, dry or sometimes heavy rain-bearing air from the Asian continent toward the Indian Ocean, significantly affecting weather in South and Southeast Asia.
NED2
Entity disambiguation (via description)
gpt-5-mini-2025-08-07
Target entity: Northeast monsoon Target entity description: The Northeast monsoon is a seasonal wind and rainfall pattern that brings cooler, dry or sometimes heavy rain-bearing air from the Asian continent toward the Indian Ocean, significantly affecting weather in South and Southeast Asia.
-
A.
Southwest monsoon
The Southwest monsoon is a seasonal wind and rainfall system that brings warm, moisture-laden air from the Indian Ocean and Arabian Sea to South Asia, producing the region’s primary rainy season.
-
B.
Indian Monsoon Current
The Indian Monsoon Current is a seasonally reversing ocean current in the northern Indian Ocean driven by the South Asian monsoon winds, significantly influencing regional climate and marine circulation.
-
C.
Madden–Julian Oscillation
The Madden–Julian Oscillation is a large-scale tropical atmospheric pattern characterized by eastward-moving pulses of enhanced and suppressed rainfall that strongly influence global weather and climate variability on intraseasonal timescales.
-
D.
La Niña
La Niña is the cool phase of the El Niño–Southern Oscillation climate pattern, characterized by unusually cold ocean temperatures in the central and eastern equatorial Pacific and associated shifts in global weather.
-
E.
Bora wind
The Bora wind is a cold, dry, and often violent northeasterly wind that blows from the interior highlands toward the Adriatic Sea, especially affecting coastal areas like Trieste.
- F. None of above. chosen
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_69a4935783b8819082b77726ec10cc42 |
completed | March 1, 2026, 7:28 p.m. |
| NER | Named-entity recognition | batch_69a49b9874c88190bd1e08d4689ea124 |
completed | March 1, 2026, 8:03 p.m. |
| NED1 | Entity disambiguation (via context triple) | batch_69a5103a30fc819086a1e95d4dfc8749 |
completed | March 2, 2026, 4:21 a.m. |
| NEDg | Description generation | batch_69a511460df4819099f70838f0f28e4b |
completed | March 2, 2026, 4:25 a.m. |
| NED2 | Entity disambiguation (via description) | batch_69a511b4b63481909b8f027726f5778e |
completed | March 2, 2026, 4:27 a.m. |
Created at: March 1, 2026, 7:33 p.m.