LAB #7 - EVOLUTION OF BOUNDARY LAYER CONVECTION
Lab Objective:
In this lab, we will examine the diurnal evolution of boundary layer convection as observed in clear-air radar data. A qualitative comparison with theoretical estimates of the type of convection that should be observed under different boundary layer conditions will be made.
Method:
1. Verify by saving a data example that somewhere around the country, at this very time, that BLC is being observed by Doppler radar.
2. Using SOLO, open one of the following two data sets:
- 02 August, 1991
- 12 August, 1991
3. Now, document the scale and type of boundary layer convection you see in the data set, from the earliest to the latest time observed.
- Save imagery to document the type of BLC, either HCRs or open/closed cells.
- Compute the aspect ratio of the observed convection. Use the soundings below to do so.
4. Now compare you observations to the theory we discussed in class.
- Does the mode of convection vary throughout the day according to theory?
- Are the computed aspect ratios consistent with theoretical values?
SOUNDINGS:
| 02 August 1991 | 12 August, 1991 |
| 1500 UTC | 1750 UTC |
| 1650 UTC | 2120 UTC |
| 2220 UTC | 2220 UTC |
last updated: Monday, November 19, 2007