What my original post asked was; if this point we commonly call "sea level" is constant then how much higher is sea level now compared to when we agreed on that standard?
The standard use of "sea level" for measuring and recording elevation is hundreds if not thousands of years old. This shows the changes in actual height of the surface since 1993:
https://oceanservice.noaa.gov/facts/globalsl.html
Any "sea level" used to measure elevation in a given area is a calculated, imposed, specified datum - it varies by location, its method of calculation varies according to need, and it is changed according to need in ways explicitly specified by those making the change.
The height above sea level of my front yard - around 900 feet, iirc, and I don't know which if any actual sea is involved - I believe has been recalculated for satellite and air travel and setting grade and so forth from the early surveys, but what they used for base and what they used as a datum for sea level I have no idea. Anyone interested in the height changes of the land itself would of course convert the old numbers to the new base (or vice versa) in step one.
I agree, in fact I believe it is the most important factor . It is a constant which can serve as a baseline?
It already is, where that's useful - such as weather reports.
Here are wind speeds and humidity readings reported by level of atmospheric pressure - with one major addition: "surface" numbers are reported as a separate layer. There is no atmospheric pressure reliably corresponding to "surface", although "1013 hPa" is generally taken as close to sea level:
https://earth.nullschool.net
Air is inconstant - famously, metaphorically, even stereotypically. Barometric pressure varies by temperature, humidity, height, and even wind formations. Notice that even careful taking of averages won't help - the ring of lows around Antarctica are fairly stable in general location, but do not correspond reliably to extra sea height, for example. Neither does the characteristic high over Siberia correspond to a gigantic dent in the planet's surface. Illustration:
https://en.wikipedia.org/wiki/File:Mslp-jja-djf.png
Notice that the "sea level" west of the southern coast of Chile, calculated from these 15 year averages and the standard lapse rate of about 12 hPa per 100 meters (Wiki), would differ from the "sea level" north of the nearest Antarctic coast by more than 300 meters.