When we first setup the theodolite we orient the instrument so that it shows an azimuth (direction) of 0 degrees when pointed to north, and an elevation (tilt) of 0 when pointed straight out. After we release the balloon we crank the azimuth and elevation so that we keep the balloon in sight. The theodolite automatically reads the azimuth and elevation for us and sends the data down a cable buried under the ice to a laptop in the building. We have a piece of computer software that then reads the azimuth and elevation every 30 seconds and computes the winds. We can do this because we know how high the balloon is every 30 seconds because of the known ascent rate. We know how high it is, and how much the azimuth and elevation have changed since the previous reading (or since the start) so simple math will let us calculate the wind speed and direction. The results are valid at the midpoint between the two levels. For example, the first level as seen in the last picture is at 150 feet above the ground. That's because the first reading is at 0 feet, and the next reading 30 seconds later is at 300 feet, so the mid point is 150 feet.
The first two pictures are of our other meteorologist down here with me, Chris. I am training him on how we forecast for balloon launches at CSBF. The next picture is a picture of the data.



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