Need help understanding pressure vs weather systems

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Discussion Overview

The discussion revolves around the relationship between pressure systems and weather phenomena, particularly focusing on the conditions necessary for rain formation and the behavior of air masses in different temperature and pressure scenarios. Participants explore various concepts related to humidity, condensation, and the dynamics of high and low pressure systems.

Discussion Character

  • Exploratory
  • Technical explanation
  • Conceptual clarification
  • Debate/contested

Main Points Raised

  • One participant expresses confusion over the basic explanations of weather systems and seeks deeper understanding, particularly regarding the conditions for rain formation.
  • Another participant suggests that high temperatures allow air to hold more water vapor, which may explain why clear skies can persist despite rising air temperatures.
  • Discussion includes the concept of low pressure systems being associated with rain, questioning how rising warm air leads to condensation and precipitation while also considering the cooling effect of rain.
  • Participants introduce the idea that moist air is less dense than dry air, which may influence pressure dynamics and the stability of air masses.
  • Links to external resources on dew point and condensation levels are provided to further elaborate on the processes involved in cloud formation and precipitation.
  • One participant mentions the importance of understanding terms like "Lapse Rate," "Lifting Condensation Level," and "Adiabatic Expansions" in relation to humidity and weather systems.

Areas of Agreement / Disagreement

Participants do not reach a consensus on the explanations for the observed weather phenomena. Multiple competing views and interpretations of the relationship between pressure systems and weather conditions remain present throughout the discussion.

Contextual Notes

Some participants reference specific conditions and examples, such as dew points and humidity levels, but there are unresolved assumptions regarding the definitions and implications of these terms in the context of weather systems.

Square1
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This is a subject that confuses me for a long time. Everywhere I go to get an understanding, I seem to run into the same explanations over and over which don't really do that much explaining. I find that only the basic elements of weather are explained, and overly basic examples that utilize them are used.

So, I would love for people to read my introductory post, answer some questions, and from there I can probably ask some follow up questions as needed to get to the bottom of some things.

I know that in the end, for rain to happen, the water in the air must condense into liquid from its vapor form..and fall down...There seem to be different ways that this can happen though.

One common explanation here is, to imagine hot sunny days (and presumably clear...) where the ground ends up heating up a lot. The surrounding air warms up, rises, and starts to cool at one point to form clouds and rain. Presumably the surface air has more water in it than upper air, so the new air can last only so long at higher altitude before its water condenses out.

(1) So how can you have a condition where it is really hot for days during the summer while the air is getting pumped into the sky, and yet, the skies remain practically clear?
(2-a) On a related note, let's say that location did end up getting rain. It is said that rain is associated with low pressure systems. Is it because as an area warms up, the air expands, pressure drops (the air is not closed off), rises, condenses, rains..etc, meanwhile the area still somehow remains relatively warm therefore the pressure is low? (2-b) But when it rains it is generally cooler than it was before. How to reconcile this? (2-c) Why in that case do we have those high pressure systems which commonly bring in heat waves or warm weather in the summers?

That's where I would like to begin. Thank you all :)
 
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Square1 said:
I know that in the end, for rain to happen, the water in the air must condense into liquid from its vapor form..and fall down...There seem to be different ways that this can happen though.

One common explanation here is, to imagine hot sunny days (and presumably clear...) where the ground ends up heating up a lot. The surrounding air warms up, rises, and starts to cool at one point to form clouds and rain. Presumably the surface air has more water in it than upper air, so the new air can last only so long at higher altitude before its water condenses out.

have a read of this from Wiki
https://en.wikipedia.org/wiki/Dew_point

particularly the section on Humidity and Dew Point. This explains how and why invisible water vapour in the air condenses and forms clouds
Square1 said:
(1) So how can you have a condition where it is really hot for days during the summer while the air is getting pumped into the sky, and yet, the skies remain practically clear?

most of that will also be answered in my link ... but briefly On those hot summer days, the air pressure and temperature will be higher and therefore the air can hold much more water vapour before condensation occurs, hence high humidity conditions ariseDave

EDIT: I did a post not so long ago with all this info in it ... still trying to find it for you
 
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Thanks. I will check these out today!
 
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Square1 said:
(2-a) On a related note, let's say that location did end up getting rain. It is said that rain is associated with low pressure systems. Is it because as an area warms up, the air expands, pressure drops (the air is not closed off), rises, condenses, rains..etc, meanwhile the area still somehow remains relatively warm therefore the pressure is low? (2-b) But when it rains it is generally cooler than it was before. How to reconcile this? (2-c) Why in that case do we have those high pressure systems which commonly bring in heat waves or warm weather in the summers?

Might it be so simple as... ?

What is density of moist air compared to dry air ? Answer lies in molecular weights and parftial pressures.
Moist air is a mix of mostly nitrogen(mw=28), oxygen(mw=32), and water vapor(mw=18),
When dewpoint is 80F (S Florida moderate but a Phoenix monsoon),
saturation pressure is ½ psia , so air is about 0.5/14.7 = 3% water vapor.
When dewpoint is 40F (S Florid unheard of but Phoenix moderate)
saturation pressure is 1/8 psia so air is about 0.8% water vapor.
A column of dry air two miles high weighs more than a moist one (at the same temperature).
So the pressure at its bottom will be higher.
To solidify the concept you should calculate by how much.
Next -
The moist column holds a lot of "heat of vaporization" that the dry one just doesn't possess. So it's more likely to be unstable and make rain clouds.

Armed with that simple observation plus your gas laws from high school chemistry class,
see if this writeup makes sense of terms "Lapse Rate " and "Lifting Condensation Level" and "Adiabatic Expansions" .
http://homepage.smc.edu/morris_pete/physical/main/notes/pg-humidity.html

i hope this helps "the light switch on" for you.
 
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