Is there a relationship between geostrophic deflection force and horizontal pressure gradient force in the journey of high-altitude wind?

The horizontal pressure gradient force is determined by the density of isobar. The denser the isobar, the greater the pressure gradient force. On the contrary, with the pressure gradient force, there will be initial wind.

The geostrophic deflection force is determined by latitude, and the equator is 0. The higher the latitude, the greater the geostrophic deflection force, and the conclusion that the poles are the largest can be drawn.

So there is no direct relationship between the two.

But they have a direct effect on the wind. Horizontal pressure gradient force affects both wind speed and wind direction. Geostrophic deflection only affects the wind direction.

What you are asking is whether the horizontal pressure gradient force is equal to the geostrophic deflection force or the influence of one large and one small on the wind. First of all, you should make it clear that in the process of wind formation and constant change, these two forces are constantly changing their direction and size, not always the same. When the two forces are balanced, that is, when the directions are opposite and the magnitude is the same, the wind direction is parallel to the isobar.