The Intertropical Convergence Zone (ITCZ) is a band of low pressure that runs around the planet Earth; The Polar front is the Arctic band of low pressure that run around 60° N and south.
Both those bands are subject to shifts and deformation due to the thermal differences and pressures and mostly are afected by the shape of the land they encounter.
The Subtropical High Zone (STHZ) instead is the correspondent high pressure area that runs around 30 degrees north and south in general between the other two types of bands.
The ITCZ is frequently bent due to pressure differences between highs;Likely so does the Polar front, but the behaviour of the STHZ... is what I'm trying to understand.
How does the STHZ deform according to the changes on the polar front and ITCZ during the seasons, if it does at all?