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I’m sorry if I’m missing something, but I’m still confused here. The subtraction I’m using follows the same principle as using addition. Depending on which reference frame I’m looking at, the operations switch. From the frame of the stationary anemometer, the windspeed it measures is 153 mph. The tornadic wind it measured would have to take into account both the translational speed of the tornado and the windspeed with respect to the tornado itself, so that 153 mph could be broken up into two components. This is because the tornado itself is moving in this frame, along with the winds.The general assumption I've seen is that the speeds are additive, which is used in, amongst other things, the interpretation of doppler radar data. This is the opposite of what you're assuming.
If I’m looking at the reference frame of the tornado itself, then the tornado is now moving at 0 mph because it is at rest in this frame. So, the only “windspeed” from this frame would be only one of the components, and it wouldn’t be the translational speed. That’s the “windspeed” I was talking about in my posts above.
But, now that I think about it, it doesn’t matter what the windspeed from the tornado’s frame is - all that really matters is what a stationary frame would experience, because that is what a home or trees would feel in the event of a tornado. So my original point is practically moot anyways.
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