Upper-Air Soundings / Stability [ Resources | Exercises]
Lab Exercises
Goals:
- Enhance understanding of thermodynamic diagrams
- Gain confidence in interpreting soundings
- Learn definitions and application of severe-weather stability indices
Method: Independent work by the students, utilizing computer spreadsheets, web-based tutorials, and other tools.
- Examine soundings and severe-weather stability indices presented on the web
- Compute selected stability indices
A. Comparison of On-line Soundings
- List the Station IDs (3 or 4 letter) and City Names of the 6 rawindsonde sites closest to your university ( UWy ).
Note that ICAO station IDs officially have 4 letters, but often the first letter is omitted if it is obvious.
The first letters most common in N. America are:
- C = Canada
- K = continental USA
- P = Alaska & Hawaii
- What are the other rawinsonde stations in your State or Province (skip this question if the answer was already fully listed in question C1)?
- Retrieve and print the current sounding for Maniwaki, Quebec (CWMW), in the following 4 thermo diagrams, and discuss how the sounding looks in each diagram:
- Skew-T (UWy - set Type of Plot to "GIF Skew-T")
- Stuve (UWy - set Type of Plot to "GIF Stuve")
- Emagram (NIU - select Emagram for station CWMW)
- Tephigram ( UQAM )
- Repeat the previous question, but for the upper air station nearest to you (except don't get the tephigram). Also, at what pressure height is the tropopause, based on the sounding you plotted.
B. Stability Indices
- How are the following stability indices defined, and what threshold value for each of them indicate a severe thunderstorm? ( NWS , and see the other links listed in the Resources section above )
- CAPE
- K-index
- Lifted-index
- Convective Inhibition (CIN)
- Helicity
- Using current stability indices.
- Use the national radar image to find a band of strong thunderstorms ( NWS , or Intellicast , UCAR/RAP ), especially in the central or SE portion of the USA.
- Then go back to the rawinsonde station map ( UWy ), select a station just SE of the line of storms, and retrieve and print the Skew-T sounding. This is normally in the unstable air ahead of the storms. (Tip: if there are no thunderstorms, such as often happens in winter, than pick Miami Florida (MFL) or San Juan Puerto Rico (TJSJ) as the rawinsonde station.)
- For this sounding, what are the values of CAPE, K-index, Lifted-index, Convective Inhibition (CIN), and Helicity? (abbreviations explained). Do these values indicate that thunderstorms are likely? (tables relating stability index to storm intensity: NWS , or see last column of page 2, from weathergraphic )
- Plot a couple of the analysis maps of key stability indices ( FSL/WRF or SPC or UNISYS ). Which parts of N. America would most likely favor strong thunderstorms, based on these diagrams?
- Compare and discuss your severe weather forecast from D3 with any warning or watch boxes that have been produced by the NWS Storm Prediction Center.
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Resources
Thermodynamic Diagrams of Current Soundings
- Skew-T Diagrams:
- Emagram / Pseudoadiabatic Chart:
- Stuve Diagrams
- Tephigrams
- ACARS/AMDARS sounding data from commercial aircraft: NOAA FSL , .
- Hodographs of wind:
- Plots soundings on the fly (world-wide) :
- UWy: soundings (Skew-T, Stuve, hodograph) by clicking on map.
- NIU : soundings (Skew-T, emagram, Stuves, or hodographs) by entering stn ID.
- Arctic soundings (U Wisc.-Milwaukee)
- Archived sounding data ( FSL )
- Station IDs for Rawinsonde sites:
- Map showing Station IDs in any continent ( UWy )
- Map showing Station IDs ( letter & number IDs) N. America ( FSU )
- Map showing NWS sounding sites ( NWS )
- List of Station ID names and numbers in N. America ( FSU )
- Station Look-up from NWS .
Blank Thermo Diagrams (useful for hand plotting)
- Blank graphs, useful for hand-plotting of real soundings:
- Sounding data in ascii text form (for plotting on blank thermo diagrams)
Tutorials and Manuals
Stability & Severe Weather Indices
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http://www.eos.ubc.ca/courses/atsc201/A201text/BrooksCole/MetSciEngr/index.html
Copyright © 2005 by Roland Stull
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