Air is far, _far_ less dense than water.
The greater the density of a substance, the more rapid the pressure changes are within that substance as one climbs or descends.
(_Specifically, this is because the substance with greater density will have greater mass for the same volume, and that greater mass means that gravity pushes it more._)
The density of dry air at sea level pressure and 0 C temperature is about 1.29 kg/m3. The density of water at 4 C temperature is about 998 kg/m3.
It only takes about ten metres of water to equal the entire weight of air in the atmosphere.
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