CAPE [J/kg] Convective Avaliable Potetial Energy
0...500 schwach
500...1000 maessig
1000...2000 stark
2000...3000 sehr stark
<3000 extrem

Cin (Convective inhibition) in J/Kg
Stärke des Deckels je größer Cin desto unwahrscheinlicher Gewitter

PW ( Precipitable water) in Kg/m^2
depth of water in a column of the atmosphere, if all the water in that column were precipitated as rain.

TT Total Totals index
< 46 keine Gewitter
46-53 vereinzelt Gewitter
53-55 lokal Gewitter
> 55 zahlreiche Gewitter

KI K-Index
< 15 keine Schauer
< 20 keine Gewitter
21-25 Schauer möglich (20-40 %)
26-30 Schauer möglich (> 40 %)
31-35 Schauer möglich (40-60 %)
36-40 zahlreiche Schauer und Gewitter wahrscheinlich (>80%)
> 40 zahlreiche Schauer und z. T. schwere Gewitter wahrscheinlich (>90%)

LI Lifted Index LI = Tenvironment(P) - Tparcel(P)
>6 very stable
1...6 sabil, keine thunderstorms
0...-2 sligthly unstable, thunderstorms possible, with lifting mechanism
-2...-6 unstable, thunderstorms likely, some severe, with lifting mechanism
<-6 very unstable, severet hunderstorms likely, with lifting mechaniss

SI S Index
46 zahlreiche Gewitter
40-45 Gewitter vereinzelt möglich
39 keine Gewitter

SW Severe WEAther Threat Index
150...300 (Slight severe
300...400 Severe storms possible
400+ Tornadic severe storms possible

LCL Lifted Condensation Level
the height at which the relative humidity (RH) of an air parcel will reach 100%

LFC level of free convection
is the altitude in the atmosphere where the temperature of the environment decreases faster than the moist adiabatic lapse rate of a saturated air parcel at the same level

EL Equilibrium Level
upper boundary of the most significant region of CAPE in the troposphere. It is the point at which a buoyantly rising parcel of air will become equal in temperature to that of the environmental temperature

Erklärung Radiosonden
Skew-T Parameters