1956
DOI: 10.1175/1520-0477-37.10.528
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The Lifted Index as a Predictor of Latent Instability

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Cited by 326 publications
(163 citation statements)
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“…Lifted Index (LI): LI (Galway, 1956) is a measure of the thunderstorm potential, which takes into account of the low-level moisture availability, and a negative index indicates the possibility of convection. It is the subtraction of the temperature of the parcel at 500 hPa from the environmental temperature at 500 hPa like the following:…”
Section: Selected Stability Indicesmentioning
confidence: 99%
“…Lifted Index (LI): LI (Galway, 1956) is a measure of the thunderstorm potential, which takes into account of the low-level moisture availability, and a negative index indicates the possibility of convection. It is the subtraction of the temperature of the parcel at 500 hPa from the environmental temperature at 500 hPa like the following:…”
Section: Selected Stability Indicesmentioning
confidence: 99%
“…The lifted (LI) index (Galway, 1956) is obtained by first raising air parcels from the surface dry adiabatically to the lifting condensation level and then moist adiabatically to 500 mb. The index is given by the temperature difference between the parcel and the environmental air at 500 mb.…”
Section: A Computed Quantitiesmentioning
confidence: 99%
“…Additionally, there were some erroneous measurements near the ground. Nevertheless, one can see the over-adiabatic ground layer with easterly winds and the southerly flow in higher levels and the latent instability (Galway 1956;Groenemeijer 2005). CAPE, calculated from a parcel from the lowest 500 m of the atmosphere, raised dry adiabatically to the LCL and moist adiabatically thereafter, is about 1,200 J kg -1 compared to a CAPE of approximately 1,500 J kg -1 calculated from the model data.…”
Section: Pre-storm Conditionsmentioning
confidence: 81%