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The "common wind" referred to here is called the "geostrophic" wind.
Explaining why it flows parallel to the isobars when driven by the
pressure gradient is a good exercise for the physicist, unless his
religion forbids belief in the Coriolis force. It also gives new
meaning to the term "equilibrium". (The equilibrium is established
between the pressure gradient force and the Coriolis force in the
frame of reference which moves with the wind.)