Not even close to being correct.
1. Compute Earth's moment of inertia.
For a sphere of uniform density, I = .4 MR²
But since Earth's density is non-uniform, the correct moment of inertia factor is .3307, hence for Earth, I = .3307 MR²
Mass = 5.97e24 kg
Radius = 6371 km
therefore I = 8.02e31 kg km²
2. Compute moment of inertia for a thin shell of water 1 mm thick
Volume of 1 km x 1 km x 1 mm of water = 1000 x 1000 x .001 = 1000 m³.
Mass of 1000 m³ water = 1e6 kg
Area of Earth's oceans: 361,060,000 km²
Mass of 1mm water added to earth's oceans: 1e6 x 3.6106e8 = 3.6106e14 kg
For a thin spherical shell, I = 2/3 MR²
Here we assume that the oceans are evenly distributed across the surface, which isn't true, but it's not far wrong.
Therefore moment of inertia of 1mm water shell = 9.77e21 kg km²
Notice already: TEN orders of magnitude difference!
3. Angular momentum is conserved. Compute angular momentum L = Iω where ω is angular velocity in radians per second. For earth, ω = 2 π / 86400.
Therefore angular momentum L = 8.02e31 2 π / 86400 = 5.83e27 kg km² rad/sec.
Assuming for convenience that polar ice is perfectly axial, its angular momentum is zero. Melting the ice adds the moment of inertia of the shell to the moment of inertia to the Earth as a whole. So post-melt moment of inertia is: 8.02e31 + 9.77e21 = 8.02e31 (plus a lot of decimals) kg km². Since angular momentum is conserved, the new tiny-bit larger moment of inertia must be balanced by a new tiny-bit smaller angular velocity.
So:
Initial angular velocity: 7.242205216643040e-5 rad/sec
Final angular velocity: 7.272205215756699e-5 rad/sec
with a difference of 8.8634e-15 rad/sec
which amounts to a longer day by a whopping 10.53 microseconds (that's millionths of a second).
Is this detectable? It's just barely within measureability limits, but it is swamped by daily effects of weather (~1 order of magnitude larger), seasonal effects (~2 orders of magnitude larger) and long-term lunar effects (~3 orders of magnitude larger). So it's lost in the noise.