free web hosting | free hosting | Business WebSite Hosting | Free Website Submission | shopping cart | php hosting

[The following is exerpted from a letter to Allen Meece.]

[Updated 4 September 2002]

 
I have compiled a graph of the upper level temperatures we can expect during the year.  The data used is all SOCA station temperature vs. altitude data from November 1, 2000 to October 31, 2001.  The spreadsheet program I use isn't capable of handling that much data, but I was able to whip up a simple qbasic program to draw the graph for me.
 
YEAR UPPER LEVEL TEMPERATURES
 
The temperature decreases roughly linearly until 16500m.  Up until this point, the temperature range over the entire year is only about 10C.  Above 17000m, the temperature begins increasing roughly linearly and the yearly variation increases to nearly 20C.  The points along the 190K line between 23000m and 29000m represent a single day's measurement.
 
This discontinuity in temperature at 16500m probably marks the tropopause,  with the region of temperature increase being the stratosphere. 
 
Upper level wind speeds are less predictable over the course of an entire year.
 
YEAR WINDS
 
The winds at each altitude vary more or less stochastically, although their range does vary with altitude.  A peak in wind velocity occurs between 15000m and 16500m, just before the stratosphere.  After the tropopause, the wind drops down to surface speeds again, creating a region of low wind force from 16500m to 20000m, then increases more rapidly with altitude.  This region of low wind force is the best place to station the VBP platform.
 
Winds of up to 160 knots were recorded at varying altitudes.  However, these gusts were measured on only three days out of the year. 
 
The regularly spaced vertical lines at 11000m, 14000m, 16000m, etc., are an artifact caused by the fact that the sounding balloon always automatically returns data upon reaching these altitudes regardless of time or conditions.  Data at these altitudes exists for every day of the year that a sounding balloon attained them, so the data at these altitudes appears denser.
 
It's important to note that all data does not exist for all altitudes on all days of the year.  Instrument failures appear common with these soundings. 
 
CME