The speed of the vertically falling snowflakes relative to the ground can be estimated by constructing a relative velocity diagram similar to Fig 3-29 or 3-30.
When driving south on a highway in a snowstorm, the snow is coming down vertically, but it is passing the windows of the moving car at an angle of 7.0° to the horizontal.
The kinematic equations for the x and y components of the motion in two-dimensional motion at constant acceleration are given by Eqs. 2 – 11a through 2 – 11c.
In the parallelogram method, the two vectors are drawn starting from a common origin, and a parallelogram is constructed using these two vectors as adjacent sides.