Atmospheric Pressure & Rain: Is It True?

  • Thread starter Thread starter darkar
  • Start date Start date
  • Tags Tags
    Pressure
AI Thread Summary
Atmospheric pressure plays a crucial role in weather patterns, particularly in relation to rain. Low atmospheric pressure is often associated with rain because it cannot hold as much moisture as high pressure, leading to condensation and precipitation. When humid air from high-pressure areas moves into low-pressure zones, it cools and cannot retain all its moisture, resulting in rain. Additionally, the balance between buoyancy and gravity influences why raindrops fall, as increased water vapor density can disrupt this balance. Overall, changes in atmospheric pressure and temperature are key factors in the formation of rain.
darkar
Messages
187
Reaction score
0
I just read a sentence from a book, It says that when the atm pressure is low, it will be raining. Is this true? If true, why the pressure drop before raining?
 
Physics news on Phys.org
Now, I'm no meteorologist, but the following should be of relevance:

1. Why does the rain fall down?
Clearly, the atmospheric pressure is unable to counteract the force of gravity acting upon the raindrops
(That is, the bouyancy force is less than the gravity force)

2. What causes the bouyancy force to become less than the force of gravity?
Since basically, balance between bouyancy force and gravity force requires balancing air density and water vapour density, one should expect the balance to be broken if the water vapour density increases.

3. If the water vapour condenses (for example becoming a fluid/solid rather than a gas),
its density should increase, and hence, the water will fall down.

4. Possibly, one mechanism of condensing the vapour would be to change the temperature.

5. However, Important:
This is speculation from my side, the actual mechanisms are probably more complicated than this.
4.
 
Because of uneven heating and other effects, our atmosphere has both low and high pressure areas. The tendency is for the air to even out these differences and thus you get air constantly moving from the high pressure areas to the low pressure areas (this creates local winds).

Another fact is that air at high pressure can hold more moisture than low pressure air can. So when this humid high pressure air moves into the low pressure air, its pressure drops, it cannot not hold as much moisture and the excess condenses out and falls as rain. The greater the difference between the low and high pressure areas, the stronger the winds and the more moist air that will pour over and the more stormy and wet weather you get. This is why a barometer can be a good indicator as to what kind of weather to expect.
 
Janus said:
Because of uneven heating and other effects, our atmosphere has both low and high Another fact is that air at high pressure can hold more moisture than low pressure air can. So when this humid high pressure air moves into the low pressure air, its pressure drops, it cannot not hold as much moisture and the excess condenses out and falls as rain.

At constant temperature, a given mass of air holds LESS water at "high" pressure than at "low" ("high" and "low" indicating Earth surface meteorological extremes). Water vapor capacity is, to first order, a function of the volume and temperature of the air mass. As an air mass is expanded adiabatically it cools enough to reduce its temperature to less than that of the dew point temperature for its water content as ONE mechanism to produce rain --- there are other rain/precipitation mechanisms that do NOT involve pressure drops.
 
I have recently been really interested in the derivation of Hamiltons Principle. On my research I found that with the term ##m \cdot \frac{d}{dt} (\frac{dr}{dt} \cdot \delta r) = 0## (1) one may derivate ##\delta \int (T - V) dt = 0## (2). The derivation itself I understood quiet good, but what I don't understand is where the equation (1) came from, because in my research it was just given and not derived from anywhere. Does anybody know where (1) comes from or why from it the...
Back
Top