Change of sea level in relation to sea ground

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The discussion centers on the relationship between sea level and the concept of "sea ground," which appears to refer to the seabed or ocean floor. It challenges the assertion that a higher sea ground leads to lower sea levels due to increased gravitational force, explaining that local gravity anomalies and isostatic equilibrium play significant roles. The conversation highlights that water levels are not uniform and can vary based on geological features and density differences beneath the surface. Additionally, the original question is deemed poorly framed, with participants suggesting that the teacher's explanation was incorrect. Overall, the complexities of gravity, density, and geological structures significantly influence sea level dynamics.
  • #31
That doesn't make sense.

I think that's a trifle harsh.
I didn't even say I agreed with the proposal, I was just trying to clarify it so we are all talking about the same thing.

In particular, unless the local surface of the sea (regardless of how it got there) is coincident with the mean level (yes I know it's the same as the geoid for practical purposes) it will experience a different gravitational acceleration ie stronger or weaker gravity, increasing from A in the direction of B in my diagram.
So if B is below mean sea level as shown then it will experience stronger gravity, simply because it is closer to the centre of the earth. It cannot be any other way.

This has nothing to do with tides or isostacy.

Similarly the sea bed below B is where it is.

My interpretation of the original proposal is that the stronger gravity at B is attributed to the extra height of mass I have noted as L in my diagram.

Again I do not say I agree with this explanation, but I think that was the original point for discussion.
 

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