Why does the dewpoint go down with increasing temperatures?

  • Thread starter Count Iblis
  • Start date
  • Tags
    Increasing
In summary, the dewpoint goes down as the temperature increases and goes back up again as the temperature goes down.
  • #1
Count Iblis
1,863
8
You can http://www.wunderground.com/history...ml?req_city=NA&req_state=NA&req_statename=NA" ) (scroll down to see the hourly observations) that the dewpoint goes down as the temperature increases and goes back up again as the temperature goes down. There seems to be an error in the data for every half hour, but I think that the data is generally correct (for other days you see the same pattern).

The dewpoint is the temperature at which you have 100% humidity, so you would expect that the dewpoint would actually increase when the temperature increases because you have more evaporation, so the air would contain more moisture. But the data seems to contradict this.
 
Last edited by a moderator:
Science news on Phys.org
  • #2
Very interesting. Plants photosynthesize best in the morning while the sun is out and before the plant leaves reach about 35 C. Photosynthesis requires water and CO2 in equal amounts to create plant matter (e.g., saccharides). Photosynthesis (in Calvin cycle) plants shuts down above 40 C because the respiration of water and CO2 equals (or exceeds?) intake, so the major photosynthesis activity is in the morning.
[EDIT] In further investigation of the dew point for various calendar days (in viewing the Table), there seems to be no real correlation of the dew point with time of day. It may have some correlation with wind direction and speed.
 
Last edited:
  • #3
As a general principle, there is no thermodynamic reason why that would be true: dry bulb temperature and dew point are completely independent of each other. And in that graph of yours, the variation in dew point temperature is quite small and you have only one cycle shown, so I don't know that you can draw a general conclusion from that. Looking at the data for my location for the last three days, shows a vague pattern in the opposite direction (dew point rising with temperature). Over the course of a single day, weather patterns have a much bigger impact than thermodynamics.

A couple of possible influences, though:

-When the temperature drops enough to get fog and dew, water condenses out of the air, lowering the dew point.
-When it is hotter outside, water will evaporate from the ground faster, raising the dew point.
-When it is hotter outside, there is more wind/convection and the mixing of low altitude and high altitude air lowers the dew point.
 
  • #4
Count Iblis said:
You can http://www.wunderground.com/history...ml?req_city=NA&req_state=NA&req_statename=NA" ) (scroll down to see the hourly observations) that the dewpoint goes down as the temperature increases and goes back up again as the temperature goes down.

I don't see that pattern at all. Ignoring the very suspect readings on the half hour, I see a fairly flat dewpoint curve. The changes I do see are much more correlated with wind direction than with temperature.
 
Last edited by a moderator:
  • #5
Count Iblis said:
<snip>

The dewpoint is the temperature at which you have 100% humidity, so you would expect that the dewpoint would actually increase when the temperature increases because you have more evaporation, so the air would contain more moisture. But the data seems to contradict this.

Yes, but as the temperature increases, the vapor pressure of water also increases, meaning the *relative* humidity will decrease (unless there is a source of water vapor via evaporation)

http://www.elmhurst.edu/~chm/vchembook/174temppres.html

The dewpoint is a measure of the saturation point of water in air, and since the relative humidity decreases as the temperature increases, the dewpoint must decrease.
 
Last edited by a moderator:
  • #6
Andy Resnick said:
The dewpoint is a measure of the saturation point of water in air, and since the relative humidity decreases as the temperature increases, the dewpoint must decrease.

Or dewpoint could stay the same, correct? Dew forms at a given temp(air is saturated).

If the air temp increases, it's ability to hold water vapor increases, relative humidity goes down. But NOT, actual amount of water in the air.

All other things, ambient pressure, total amount of water vapor in the air, etc, remaining the same....if possible.

That dewpoint(temp) could remain unchanged, all we need to do is lower the temp again to that already defined dewpoint.

My point is dewpoint(temperature) is not dependant on ambient temperature, it IS dependant or defined by ambient pressure and actual "amount" of water in the air.

Correct?

Thanks, John
 
  • #8

FAQ: Why does the dewpoint go down with increasing temperatures?

Why Does the Dewpoint Go Down with Increasing Temperatures?

The relationship between temperature and dewpoint is an essential aspect of meteorology and plays a significant role in weather phenomena. Let's address some common questions about why the dewpoint decreases as temperatures rise:

Q1: What Is the Dewpoint?

The dewpoint is the temperature at which air becomes saturated with moisture, leading to the condensation of water vapor into liquid water, such as dew, fog, or clouds. It is a crucial parameter in meteorology for understanding humidity levels in the atmosphere.

Q2: How Are Temperature and Dewpoint Related?

Temperature and dewpoint are related through the concept of relative humidity. When air is at its dewpoint temperature, it is saturated with moisture, and the relative humidity is 100%. As air temperature increases, the dewpoint remains constant or increases at a slower rate, leading to a decrease in relative humidity.

Q3: Why Does the Dewpoint Go Down with Increasing Temperatures?

The dewpoint goes down with increasing temperatures due to the inverse relationship between temperature and relative humidity. Here's why:

  • Warm air has a higher capacity to hold moisture (water vapor) than cold air. As air temperature rises, it can "accommodate" more water vapor without reaching saturation.
  • Conversely, when air cools, its moisture-holding capacity decreases. If the temperature drops to or below the dewpoint, the air becomes saturated, and dew or condensation occurs.
  • Therefore, as temperatures increase, the relative humidity decreases because the air's ability to hold moisture increases, making it less likely to reach saturation.
This phenomenon explains why hot, dry climates often have lower relative humidity compared to cooler regions.

Q4: How Is Dewpoint Used in Weather Forecasting?

Meteorologists use dewpoint to assess the moisture content of the air and to make predictions about weather conditions. A rising dewpoint can indicate increasing humidity and the potential for precipitation, while a falling dewpoint suggests drier conditions.

Q5: Can Dewpoint and Temperature Ever Be Equal?

Yes, dewpoint and temperature can be equal under specific conditions. When the air is saturated with moisture, the dewpoint and temperature are the same, resulting in 100% relative humidity. This scenario often occurs during the formation of dew, fog, or clouds.

Q6: Are There Practical Applications of Dewpoint and Temperature Relationships?

Yes, the relationship between dewpoint and temperature is essential in various fields, including agriculture, aviation, and construction. Knowing the dewpoint temperature helps professionals make decisions related to irrigation, aircraft takeoff and landing, and preventing condensation in building structures.

In summary, the dewpoint decreases with increasing temperatures because warm air can hold more moisture before reaching saturation. Understanding this relationship is crucial for weather forecasting and has practical applications in different industries.

Back
Top