baroclinic instability model
C46003
concept
A baroclinic instability model is a conceptual or mathematical framework that describes how horizontal temperature gradients and vertical wind shear in a rotating fluid (such as the atmosphere or ocean) can lead to the growth of large-scale waves and eddies.
All labels observed (1)
| Label | Occurrences |
|---|---|
| baroclinic instability model canonical | 1 |
Description generation (CDg)
The one-sentence description above was generated by prompting gpt-5.1 with the class name and this instruction.
Instruction
generate a one-sentence description for a given conceptual class. # Response Format Return only the sentence: "Description: [one-sentence description of the conceptional class]"
Input
Class: baroclinic instability model
Generated description
A baroclinic instability model is a conceptual or mathematical framework that describes how horizontal temperature gradients and vertical wind shear in a rotating fluid (such as the atmosphere or ocean) can lead to the growth of large-scale waves and eddies.
Instances (1)
| Instance | Via concept surface |
|---|---|
| Eady–Eliassen model | — |