My problem with air presure is why it has no obvious OW. It has a pressure, but is that the same thing? I don't think so, as an OW is measurable downwards only (or more exactly, only relative to the direction of movement induced by the gravitational force). If I place a solid such as my 1kg steel ball on a scale, my scale reads its OW as 1kg. If I place my scale on the side of my ball, it measures nothing. And if I place it on top, I am measuring the weight of my scale.
But with the atmosphere, my scale will register nothing in any orientation. This is, as is well known, because the air everywhere has the same pressure so there is the same force pushing up under the scale as down. If I create a measuring device that reacts to the atmospheric pressure, I think it is totally ignorant of its orientation - that is, it will measure the same pressure regardless of which way its measuring surface faces. Atmospheric pressure is the same in all directions at any given level of the atmosphere.
However, the air has weight - it must as it has mass and there is gravity. In this thread it has become clear to me that the effect of gravity on a gas is to increase, on average, the number of molecules at each level. Disregarding effects of temperature, gravity creates a pressure gradient and that is expressed as an increase in measured pressure at each level as we come closer to the source of the gravity (I know that's not technically correct, I think I mean closer to the centre of mass between the two things).
Now, this must also happen in a solid. If I have a large column of some material, as sophiecentaur noted earlier, the force of gravity is expressed throughout that column and the pressure builds internally and can even deform the column at its lower extremity.
However, that internal pressure, and the internal deformation, is not weight in the OW sense. The column will weigh the same regardless.
This is where I had an idea about what we are seeing happen. It seems to me that for OW to be expressed, we need a bounded object. That is, our object has to have a boundary which is able to be acted upon by another boundary. In the case of the solid, say my 1kg ball, it has a surface and that surface can rest upon another surface - that prevents the ball accelerating and the force is expressed on the second surface as OW. Internally of course the force is being propagated throughout the structure via the atomic/molecular bonds.
Now, I *think* this means that inside a solid, we have an internal pressure resulting from gravity that is largely the same as the internal pressure in a volume of gas. In other words, internally we see pressure at every 'level' in the solid, and taken over its whole form there is a pressure gradient. Hence a tall column of material will have a lower internal 'pressure' at the top than at the bottom. If I could measure that pressure, I'd find that at the top of the column it is less than at the bottom, but that at any level it would be the same to the top, side or bottom of my layer, or slice.
Cumulatively, the pressure builds as we come down the column closer to the centre of mass between our two objects. At the very bottom, it could have enough force to deform the object.
Again though, this is not the weight of the object, rather it is the internal pressure. The weight, or operational weight at least, cannot be measured directly from the prssure, that can only be done outside the boundary of the object. I would imagine though that the relationships are such that we could calculate the weight from the various properties including the pressure at the very lowest layer.
Now, this leads me to assume that if my object were in free fall, ie accelerated by a local gravitational field, it has GW but no OW, and hence no pressure gradient internally. That is, the deformation sophiecentaur describes in my stationary column on the Earth's surface, does not occur. This I think is broadly analogous to the notion that my container of gas, in space, loses its pressure gradient and becomes homogenous throughout.
So that makes sense to me. What of the weight of my atmosphere?