Lifted Index from 500 hPa Temperatures
Calculate lifted index from supplied environment and parcel temperatures at 500 hPa, keeping the parcel method and index limitations explicit.
Use this result well
- Inputs that matter
- Environment temperature at 500 hPa (°C), Lifted-parcel temperature at 500 hPa (°C), Sources and assumptions
- Output to expect
- Lifted index from actual 500 hPa temperatures
- Check the units and required inputs before comparing results.
- Keep the assumptions with a copied result so you can reproduce the calculation later.
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Reference & details
How it works
Updated September 2026
How it works
Updated September 2026Lifted index from actual 500 hPa temperatures
Subtract a documented lifted-parcel temperature at 500 hPa from the environment temperature at the same pressure. Retain how the parcel origin and ascent were chosen instead of assigning an arbitrary storm severity from one index.
LI = Tenvironment,500 − Tparcel,500, in °C temperature difference.Updated: September 2026
Example Scenarios
Inspect the example and its input basis, then substitute your own documented measurements or matched cases.
→ 5°C lifted index
Common Mistakes to Avoid
Common Mistakes to Avoid
Mixing observation and model inputs
Use the exact units, timestamp, level and measurement or model basis stated by the selected mode. A similar quantity from another instrument or product is not automatically interchangeable.
Treating an illustrative case as a measurement
Replace the example with your own sourced inputs. Retain missing values and method limits, and keep raw source data alongside a saved calculation.
FAQ
About Lifted Index from 500 hPa Temperatures
Subtract a documented lifted-parcel temperature at 500 hPa from the environment temperature at the same pressure. Retain how the parcel origin and ascent were chosen instead of assigning an arbitrary storm severity from one index.