Humid air is lighter than dry air. The two hydrogen molecules in H2O make the molecul lighter than air’s other constituents. We’ve all read and heard about how the fog was thick, the humid air was heavy and so forth. This is the epitome of literary license. Trust me, dry air is heavy air.
There are many units of measure to express the pressure of air at a point on earth. I commonly use pounds per square inch largely because I’ve use Imperial measurements all my life (over 70 years) and am MUCH more comfortable with them, well with most of them. Show me someone comfortable with the slug and I’ll show you a better man than me.
Sea level atmospheric pressure in different units of measure:
PSIG 14.7 PSI
Bar 1 Bar
Millibar 1013.25
Pa ~101,325?
Hpa 1013.25
Torr (mmHg) 760
Inches Hg 29.92
During the days of sailing ships the mercury manometer was the only reliable instrument and could even be manufactured and calibrated on-board ship at sea with a sealed glass tube and some mercury (probably from the broken manometer.) The nautical necessities of centuries past continue to this day so barometric pressure is most often expressed in inches of mercury or inHg.
Barometric pressure is a common measure of the water in the air. High pressure, over about 30 inches of mercury indicates means that there is little water in the air making it heavy. Low pressure, under 30 inches of mercury, means the air is humid, making it light.
Hurricane air pressure and forecaster isobar charts are often expressed in millibars (mb) or Hectopascals (hPa).
Most weather occurs in the bottom 1,000 ft of altitude. The worst tornadoes work within a couple of hundred feet of the ground. Some of the strongest tornadoes utilize buoyant air from less than 10 feet above the ground.
Ground level pressure is the result of all the air pressure above a point. The air pressure at sea level is 14.7 Pounds per Square Inch Gauge[i] (PSIG) of air, more or less. This means there is 14.7 pounds of air above each square foot of ground or water at sea level.
Air pressure at 1,000 ft altitude is about 14.2 PSIG. A one-foot square column of air between 0 ft altitude and 1,000 ft altitude weighs 0.5 PSI. Therefore, the bottom 1,000-foot column of air at sea level weighs about 0.5 pounds (14.7 PSIG – 14.2 PSIG) or 3.5% of the air.
Thus, it follows that the bottom 3.5 % of the atmosphere is responsible for local weather.
It turns out that the change in buoyancy of dry air between 20 degrees C and 35 degrees C is about 3.5%. Nothing sinister but I bet you’ll remember those two numbers.
That value will be helpful while discussing and understanding air buoyancy in later topics.
[i] Author’s note –
The gauge suffix indicates the pressure value is referenced to a vacuum such as in outer space. This is sometimes absolute pressure.