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so now what I want to do is I want to show you on a weather map what that looks like and this section would be very important especially when it comes to forecasting upper-level winds and high and low pressure systems in the future so here when we take our previous example on our Ridge out on the west coast our trough down in the central plains and then our Ridge out towards the east coast what you notice is here you have a deep trough over the central plains well whats important is is that if you take the bottom most portion of this trough which is known as the trough access and you cut it in half in meteorology we like to say that our area of divergence is on the right-hand side which these are upper level winds because this is a 500 millibar map so if air is diverging aloft that means its converging at the surface and so what does that mean that means we have an area of low pressure that is somewhere in this black circle and over on the left-hand side of the trough axis we have ou
