hot
Yes, water can condense while boiling, particularly at the surface of the liquid or on cooler surfaces nearby. When water boils, it turns into steam (water vapor), and if this vapor comes into contact with a cooler surface, it can lose energy and condense back into liquid water. This is often observed as droplets forming on the sides of a pot or lid during boiling.
The liquid that condenses on glass when you breathe on it is water. The water is a condensate, and the cooler glass causes water in air we exhale to cool and condense.
If convection currents did not form in the surface zone of a body of water, the water temperature would likely become more stratified and less uniform. Warmer water would remain at the surface, while cooler water would settle below, leading to reduced mixing. This could result in localized areas of warmer or cooler temperatures, negatively impacting aquatic life and nutrient distribution. Overall, the absence of convection currents would disrupt the natural thermal balance of the water.
Misty fogs form when water boils because the hot water vapor comes into contact with cooler air, causing it to condense into tiny water droplets that we see as mist. This process occurs when the warm air, saturated with water vapor, meets a cooler surface, leading to condensation and the formation of mist.
Fog forms when the air near the ground cools and reaches its dew point, causing water vapor to condense into tiny water droplets. This process can occur when warm, moist air comes into contact with a cooler surface or when the air cools at night.
Yes, water can condense while boiling, particularly at the surface of the liquid or on cooler surfaces nearby. When water boils, it turns into steam (water vapor), and if this vapor comes into contact with a cooler surface, it can lose energy and condense back into liquid water. This is often observed as droplets forming on the sides of a pot or lid during boiling.
Yes, water vapor can condense onto a cooler water droplet because condensation occurs when water vapor loses heat energy and changes back into liquid form upon contacting a cooler surface. This process can be observed in the formation of clouds or fog when water droplets in the air cool down and collect water vapor.
Yes, water vapor can condense on trees when the temperature of the tree surface is cooler than the dew point temperature of the air. This can happen during cool nights or when trees are shaded from the sun. The condensed water droplets appear as dew on the tree's surface.
It may condense into clouds, or into precipitation, because cooler air cannot hold as much water vapor as warmer air.
Yes, warmer water generally has less oxygen compared to cooler water because oxygen dissolves more easily in cooler water.
cooler
Yes, when you breathe on a mirror, the warm water vapor in your breath condenses on the cooler mirror surface, causing it to fog up. This is an example of condensation where a gas (water vapor) turns into a liquid (water droplets) upon contact with a cooler surface.
During summer, the sun heats the surface of the pond more quickly than the deeper layers due to direct sunlight exposure. This results in the surface water feeling warmer. Conversely, the deeper layers of the pond remain cooler as they are not in direct contact with the sun's heat, creating a temperature difference between the surface and the bottom.
The sun heats the water surface. Warm water has a lighter density than cold water so the warmer water floats on the surface of the colder water.
cooler
When we boil water and expose the steam (water vapor) to a cold surface, it will condense into tiny drops of water on the cold surface. If you can see the 'steam'rising above the water, it has already condensed into tiny droplets of water in the cool air.
The sun heats the water surface. Warm water has a lighter density than cold water so the warmer water floats on the surface of the colder water.