This chart shows a cyclone in the Southern hemisphere. Draw the center location of the low-pressure area, the approximate isobar contours around it. The Pressure Gradient Force points
(Outward, Inward, Along the isobars counter clockwise or clockwise)
,and the Coriolis Force points
(same options)
.Since the winds (shown here: stream lines) have a curvature, the Coriolis Force needs to be slightly
(Weaker, or Stronger)
than the opposite Pressure Gradient Force.