I simply presumed that water that's pumped from layers 100m or lower below the surface, water that's sometimes 10.000 years "old", wasn't surface water. But it makes sense to lump it in there too.
The breakout is for comparison: surface freshwater (total) and surface freshwater (lakes and rivers) relatively.
That one actually has percentages on the subsets too for interesting differences like glacier and icecap volume vs ground water (which I think still excludes the kind of deep mantle water mentioned up thread because it's not usably extractable).
Is the water pumped from beneath the crust in the Netherlands poisoned too or have you guys got the last of the good stuff?