Used to plot the vertical distribution of temperature, dew-point, and pressure obtained by a radiosonde
It creates a vertical profile of the atmosphere!
Radiosondes can obtain data up to a height of around 30 km
Skew-T = Isotherms (see left image below)
Lines of equal temperature that are slanted or skewed
Log-P = Isobars (see right image below)
Lines of equal pressure that are spaced logarithmically
Each data point is plotted and then connected with a line
Image Description: Skew-T Log-P (Isotherms)
Pressure (mb) is recorded to the left of the graph. Temperature (C) is recorded on the bottom (x-axis) and is repeated around the right y-axis.
*Note: the lines are of constant temperature, so whether you are looking at them from the x or y axis shouldn't matter, as each line has its value repeated.
Isotherms in this image are highlighted as teal diagonal lines, crossing the isobars
Image Description: Skew-T Log-P (Isobars)
Pressure (mb) is recorded to the left of the graph. Temperature (C) is recorded on the bottom (x-axis) and gets wrapped around the right y-axis.
Isobars in this image are highlighted as orange horizontal lines, crossing the isotherms
Reminder: Td should never be greater than T!
Inversion: Any segment in the troposphere where temperature increases with height
Possible Cloud Layers: Any segments where the difference between the temperature and dew point temperature is 5ºC or less
Freezing level: The level at which the temperature drops below 0ºC
If the entire temperature profile is below zero, the freezing level is reported at the surface (usually 100mb).
Tropopause Height: Boundary between troposphere and stratosphere, where the temperature increases with height.
Look just below where the temperature starts increasing at the top of the atmosphere
Winds can also be plotted on a sounding to visualize how wind is changing with height (see example sounding below)
Wind barb is the direction the wind is coming from, given in degrees