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Would be interesting to see some mathematical evidence on two last posts 
Anyway - as the wind (in Denmark anyway) will never be constant for a sustainable period of time (and add on top of that turns, going north, going south, etc), believe it must be rather chaotic (as with most fluid physics).
However, fact is that the drag (or wind resistance if you will) initially (and in it's most simple form) is determined by the cross sectional area of the specified item, and the square of the velocity ... so going slower should decrease drag, but not necessarily get you get to T2 faster 
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