Limitations of temperature in a large body of water

  • Context: High School 
  • Thread starter Thread starter sgstudent
  • Start date Start date
  • Tags Tags
    Body Temperature Water
Click For Summary

Discussion Overview

The discussion revolves around the limitations and complexities of measuring temperature in large bodies of water, specifically rivers and lakes. Participants explore how temperature is defined and measured, the effects of water movement on freezing, and the challenges of achieving uniform temperature readings in such environments.

Discussion Character

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

Main Points Raised

  • Some participants propose that in flowing water, like rivers, the mixing of warmer water from the depths prevents freezing at the surface, while others question how temperature is measured in such dynamic conditions.
  • There is a discussion about whether temperature readings from thermometers in large bodies of water reflect the average kinetic energy of all molecules or just those in immediate contact with the thermometer.
  • One participant notes that measuring temperature in large bodies of water is complicated by the presence of localized variations, such as frozen eddies and warmer currents.
  • Some participants express uncertainty about what constitutes the "average" temperature in a large body of water and how to accurately quantify it.
  • A later reply mentions the idea of monitoring radiation from a large body of water as a potential method for obtaining an overall temperature, highlighting the difficulties in achieving a consensus on temperature measurement.

Areas of Agreement / Disagreement

Participants generally agree that measuring temperature in large bodies of water is complex and that localized variations exist. However, there is no consensus on the best method for measuring or defining temperature in these contexts, and multiple competing views remain regarding the implications of these measurements.

Contextual Notes

Limitations include the dependence on the definitions of temperature, the challenges of achieving uniform temperature in large volumes of water, and the unresolved nature of how to quantify temperature in such scenarios.

sgstudent
Messages
726
Reaction score
3
In a river, water flows so how does it resist freezing? Or does it freeze at the same rate just that at the point where the cooling agent is at, the water keeps getting replaced. So the average kinetic energy of all the water molecules drop so as a whole the temperature drops?

But a river is huge so if I place a thermometer in one area and then in another, there's a good possibility that the 2 readings are different. So I'm quite confused about how temperature works. Temperature is the average kinetic energy of all the molecules but what are the limits to this?

Thanks for the help :smile:
 
Science news on Phys.org
I'm not quite sure I understand your question but...

On a lake heat is lost to the atmosphere and that allows the temperature of the top surface to fall to freezing point while the depths remain warm(er). The surface of a river tends not to freeze because of mixing with warmer water from the depths.
 
CWatters said:
I'm not quite sure I understand your question but...

On a lake heat is lost to the atmosphere and that allows the temperature of the top surface to fall to freezing point while the depths remain warm(er). The surface of a river tends not to freeze because of mixing with warmer water from the depths.

sorry for being vague. What i meant was what is temperature measuring actually? When we put our thermometer into a small tub of water, we find the average KE of the molecules of all the water molecules? Then what about a large body of water like a river, when we place our thermometers into it what are we measuring now?
 
When you use a thermometer, you are measuring the temperature of the substance directly in contact with the device. In general, it takes special care to ensure that temperature is uniform in a given mass of a substance, whether it is solid, liquid, or gas. In bodies of water like rivers and lakes, it is very difficult to make the temperature of the water uniform throughout.
 
SteamKing said:
When you use a thermometer, you are measuring the temperature of the substance directly in contact with the device. In general, it takes special care to ensure that temperature is uniform in a given mass of a substance, whether it is solid, liquid, or gas. In bodies of water like rivers and lakes, it is very difficult to make the temperature of the water uniform throughout.

But technically what is the substance directly in contact with the thermometer? Are they just those few molecules around it? But if that's the case how can it be because isn't temperature the average KE of all the particles? That causes a new problem too, as what would quantify 'all' the particles present.

Hope you can help out :smile:
 
Are they just those few molecules around it?
I would not call something like 1020 (give or take some orders of magnitude depending on the type of measurement) "a few", even if it is a tiny fraction of 1 liter.
But if that's the case how can it be because isn't temperature the average KE of all the particles?
You measure the average kinetic energy of those 1020 molecules, which is the temperature of them = the temperature directly at the thermometer.
 
mfb said:
I would not call something like 1020 (give or take some orders of magnitude depending on the type of measurement) "a few", even if it is a tiny fraction of 1 liter.
You measure the average kinetic energy of those 1020 molecules, which is the temperature of them = the temperature directly at the thermometer.

Oh that explains why its so difficult to freeze running water, the molecules around the cooling agent leaves before enough energy is removed from them?
 
You point out that the very idea of a temperature is not readily applied to anything big or fluid, such as a lake or a river.
Temperature applies to one locale at one moment, how big and long depends on the sensor and the measurement interval.
So the river may have frozen eddies and warmer stream runs at the same time. As it freezes over, your measurement space shrinks as well.
The only way to get an overall temperature is to moniter the radiation from the object in question. Otherwise, confusion reigns, as with global warming today.
Al Gore had championed a satellite at one of the LaGrangian points that would observe the entire Earth at once from about 1.5 million miles away and measure its temperature. Unfortunately, that was not funded, so there is still no broadly agreed measure, just lots of local thermometers with lots of adjustments.
You too will need lots of adjustments to measure your river temperature, but don't feel bad, everyone else has the same problems.
 

Similar threads

  • · Replies 16 ·
Replies
16
Views
7K
  • · Replies 32 ·
2
Replies
32
Views
4K
  • · Replies 3 ·
Replies
3
Views
2K
  • · Replies 3 ·
Replies
3
Views
3K
  • · Replies 10 ·
Replies
10
Views
2K
  • · Replies 5 ·
Replies
5
Views
4K
  • · Replies 16 ·
Replies
16
Views
2K
  • · Replies 7 ·
Replies
7
Views
3K
  • · Replies 3 ·
Replies
3
Views
2K
  • · Replies 1 ·
Replies
1
Views
2K