The total volume of water increases both due to melting of on-land ice and thermal expansion of the water column - however it is the case that the resulting increased volume is not evenly distributed, due to the factors I mention above.
If you're getting at "crustal thickness" - there are areas of thin or less dense crust where the value of g is lower by a tiny amount - but this tiny amount is enough to cause less water to gather in that area over the vast depth of the water column, as it's essentially uphill to there.
https://en.wikipedia.org/wiki/Gravity_of_Earth#Local_topogra...
https://en.wikipedia.org/wiki/Gravity_anomalies_of_Britain_a...