Ridges of high pressure between depressions usually move in the same direction as the depression, but anti-cyclones formed behind a cold front usually move with the cold air.
Imimango yoxinzelelo lomoya oluphezulu phakathi kokuhla koxinzelelo lomoya lusoloko luhamba ngendlela efanayo njengokuhla koxinzelelo lomoya, kodwa ezingeyo nkanyamba zenzeka emva kwengqimba zomoya obandayo zisoloko zihambe nomoya obandayo.