SkyStef's weather page |
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SSI > 2: no thunderstorms. (*) To find 500 hPa parcel temperature: construct LCL for parcel at 850 hPa. From this point ascend saturated adiabatically to the 500 hPa level and read off. This Index doesn't work well if a frontal surface or inversion is present between 850 hPa and 500 hPa.
Formula used: SSI = T - Tparcel (both T at 500 hPa) |
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