• # Is moist air heavier or dry air heavier?

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Generally we assume that moist air is heavier and dry air is lighter. In that sense dry air must go up and moist air should stay at the lower strata of the atmosphere. But in reality the water vapor evaporated from water bodies will rises up to the higher levels of atmosphere and get condensed to precipitate as rain. If it is true, why moist air but not dry air raising up to higher level of atmosphere and get condensed to precipitate as rain. Any body give logical explanation for this phenomenon.
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• The molar mass of water vapors H2O is 18 whereas the molar mass of dry air is 28.57, taking into account about 78% nitrogen, N2, 21% oxygen, O2 and 1% other gases. According to the Avogadro's Law, a molar mass of air and water vapor will occupy the same volume i.e. 22.414 litres. Thus the density of water vapors 0.804 g/L is much lower than the density of dry air which is 1.27 g/L.

Therefore contrary to the popular belief, the density of humid air is lower than that of the dry air which causes the humid air to go upward.

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• The weight or mass of a material decides whether it is heavier or lighter. Again the mass depends on the molecular mass of that material. As per atomic theory, one mole (6.023 * 10?23 molecules) of a material have definite volume of 22.4 litres and for this constant volume its weight (mass) is molecular mass of that material. Hence, material having greater molecular mass will be heavier than the material having lower molecular mass. Further, the chemical composition of a material decides its molecular mass. If we go for chemical composition of dry air, it is a mixture of various gases. Hence its molecular mass will depend on the molecular mass of all gases present in it. Nitrogen (78%) and oxygen (21%) are the major component of dry air. The molecular mass of Nitrogen is 28 and that of Oxygen is 32. Hence if we calculate the molecular mass of dry air by ratio calculation method, then it will come around 29. The moist air contains water component in varied percentage. The molecular mass of water (H2O) is 18). Now again we calculate the molecular mass of moist air, it will come towards lower side because the molecular mass of water is lower than the molecular mass of dry air. With increase in water percentage, the molecular mass of air will slowly start decreasing. Thus we can conclude that the dry air is heavier than moist air.

• Usually people believe that moist air is heavier than dry air. They feel since the moist air carries a lot of weight due to moisture present in it should be heavier when compared to dry air without any trace of moisture or humidity in it. However, this is not true. Dry air is heavier when compared to moist air. Moist air carries more water molecules. This result in displacing molecules of oxygen and nitrogen. A water molecule weighs approximately 36% less than that of Nitrogen molecule and approximately 44% less than that of oxygen molecule. Thus, as more and more moisture accumulates in the air, the more and more lighter it starts to weigh.

Since moist air is lighter will condense and rise up to high level of atmosphere and not dry air. Water evaporates from water bodies on earth and the air over that particular water body becomes moist and thereby becomes light in weight. Surrounding air is dry and thereby weighs more. This creates an unstable situation. As more and more moist air keep on accumulating, it altogether as a single packet escapes the surface of earth and rises above and do not get mixed with the surrounding dry air that is not carrying any moisture in it. It thereby condenses and precipitate as rain.

• When temperatures climb into the 90s with high humidity levels (dew points in the 70s), one is likely to hear someone say: 'The air is really heavy today.' Or, maybe, given today's low humidity, one may think that air seems particularly light.
But, assumption that humid air is heavier than dry air is wrong.
In very hot, humid weather, one may feel that air is heavier because moving around seems to take more energy on dry days. Sticky days feel 'heavier' because heat and high humidity slows evaporation of perspiration, body grows hotter and this saps one's strength.
One may also say: 'Water is heavier than air.' True, a glass of liquid water weighs more than a glass filled only with air. But, humidity is water vapour, not liquid water and water vapour molecules are lighter then molecules of nitrogen and oxygen which make up about 99% of the atmosphere.
At this stage, one could argue: 'It does not make any difference that water molecules are lighter than those of oxygen and nitrogen. Water molecules are being added to oxygen and hydrogen in air, which make it heavier. One would be wrong. To see why, we need to go back to 1811 and work of Italian scientist Count Lorenzo Avogadro, who hypothesized that equal volumes of gases at same temperature and pressure contain equal numbers of molecules.
By 1860, Avogadro's law was a bedrock of chemistry as it still is.
In other words, when water molecules evaporate into a cubic foot of air, an equal number of other molecules will leave that particular cubic feet of air.
Each molecule of water which evaporates into a particular parcel of air as vapour will replace a molecule of either nitrogen or oxygen, which accounts for roughly 99% of air's gases. Nitrogen in air has molecular weight of 28% and oxygen molecule has molecular weight of 32%.
Water vapour molecules, which are one oxygen atom with a weight of 16 and two hydrogen atoms each with a weight of 1, add up to a molecular weight of 18, which is much lighter than the nitrogen and oxygen they displace when they evaporate into air.
For example, at both 3:52 and 4:52 p.m. on July 19th 2013, temperature at National Airport was 94 degrees and dew point 74 degrees. This combination made air's density 0.0708 pounds per cubic foot or in metric system 1.134 kilograms per cubic meter.
On a very dry day, with same 94-degree temperature and atmospheric pressure as on 19th but a dew point of only 50 degrees, air's density would have been 0.0712 pounds per cubic foot or 1.141 kilograms per cubic meter.
There are three ways of turning moist air into cloud so that it rains or snows.
Rain and other forms of precipitation occur when warm moist air cools and condensation occurs.
Since warm air can hold more water than cool air, when warmer air is cooled, moisture condenses to liquid and it rains.
Frontal rain occurs when two air masses meet. When a warm air mass meets a cold air mass, they don't mix as they have different densities. Instead, the warm less dense air is pushed up over cold dense air creating the 'front'. As a result, much like when air is forced up over mountains, warm less dense air cools and water vapour condenses into water and falls as raindrops. This type of rain can happen anywhere in the UK.
Orographic rain:
Orographic rain is rainfall produced as a result of clouds formed from topography or shape of the land. Where there is high ground, moist air is forced upwards producing cloud and precipitation.
Mountainous areas close to prevailing westerly winds are most likely to experience this type of rainfall. Geography of the UK means that this type of rainfall is most common in the north and west of the UK where warm moist air from Atlantic cools as it is forced upwards over high altitudes.
Convective rain:
Convective rain is produced by convective cloud. Convective cloud is formed in vertical motions which result from instability of atmosphere. One way that atmosphere can become unstable is by heating from the sun, ground warms up, causing moisture in the ground to evaporate and rise and hot ground too heats the air above it. As water vapour rises, it cools and condenses into clouds and eventually rains.
When you heat the air from below, much like in boiling kettle, you tend to get 'bubbles' of rising air, known as updraughts. These are smaller than large-scale lifting of air which occurs at fronts and over mountain ranges. This tends to give us smaller areas of rain, with clear spells in between, referred to in the UK as 'sunshine and showers'.
This type of rainfall is common in the south and east of the UK, where it is warmer. This area is also prone to very heavy showers because warmer air can hold more water.
Sometimes, one can get all three types of rain at one time and this can lead to severe flooding.

• Moist air has water vapors contained in it and because of this its density is higher than equal volume of dry air which has theoretically no water vapors in it. Thus moist air is of higher weight than dry air.
Dr. Paresh B. Gujarati.
Mechanical Engineer.
'I'mprovement always begins with 'I'.

• We know that hot air is lighter than cold air. Moist air is heavy than dry air. Sometimes moist air turns into fog and it has higher density than dry air. Water vapours created due to heat. It is lighter than moist air. At this time water droplets have kinetic energy, K.E.=1/2 mv2. This energy also helps water vapours to go rise.

• As a matter of first importance, "damp air" will be air with a high water vapor content. Water vapor, the undetectable, vaporous type of water, happens in exceedingly factor sums in the air. Water is made out of a hydrogen iota and two oxygen iotas (H2O) and has an atomic weight of 18 grams for each mole. (One mole of a gas, at standard conditions, has a volume of 22.4 liters.)

"Dry" air contains no water vapor, and is for the most part a blend of sub-atomic nitrogen (N2) and sub-atomic oxygen (O2). The sub-atomic weight of dry air is 28.97 grams for each mole.

Since mole per mole, dry air is heavier than water vapor, any blend of dry air with water vapor will weigh not exactly unadulterated dry air. The more water vapor noticeable all around, the littler its atomic weight will be.

Consequently the thought that damp air is heavier than dry air on a late spring night at the ballpark strikes out when contrasted with the physical reality

Some times peace is better than being Right!!!

• The simple logic behind the rising of moist air is that it contains more amount of water molecules compared to dry air. The process of evaporation is responsible for the rising of moist air.