Stratification is defined as the layering of water caused by temperature. I guess you are talking about condensation. Condensation is the transition of gas to liquid, the opposite of boiling.
Sometimes it happens that there is a layer of water on objects caused by temperature. This happens when warmer air which contains water in gas from makes contact to a much cooler surface like a cold window or mirror, causing the water to condensate back to liquid form.
This same principle causes dew in the morning.
Thermal stratification is the term that describes the layering of water caused by differences in temperature. This phenomenon is common in lakes and oceans, where warmer, less dense water floats on top of cooler, denser water, creating distinct layers based on temperature.
Stratification is defined as the layering of water caused by temperature. I guess you are talking about condensation. Condensation is the transition of gas to liquid, the opposite of boiling.Sometimes it happens that there is a layer of water on objects caused by temperature. This happens when warmer air which contains water in gas from makes contact to a much cooler surface like a cold window or mirror, causing the water to condensate back to liquid form.This same principle causes dew in the morning.
Stratification is defined as the layering of water caused by temperature. I guess you are talking about condensation. Condensation is the transition of gas to liquid, the opposite of boiling.Sometimes it happens that there is a layer of water on objects caused by temperature. This happens when warmer air which contains water in gas from makes contact to a much cooler surface like a cold window or mirror, causing the water to condensate back to liquid form.This same principle causes dew in the morning.
Stratification is defined as the layering of water caused by temperature. I guess you are talking about condensation. Condensation is the transition of gas to liquid, the opposite of boiling.Sometimes it happens that there is a layer of water on objects caused by temperature. This happens when warmer air which contains water in gas from makes contact to a much cooler surface like a cold window or mirror, causing the water to condensate back to liquid form.This same principle causes dew in the morning.
Stratification is defined as the layering of water caused by temperature. I guess you are talking about condensation. Condensation is the transition of gas to liquid, the opposite of boiling.Sometimes it happens that there is a layer of water on objects caused by temperature. This happens when warmer air which contains water in gas from makes contact to a much cooler surface like a cold window or mirror, causing the water to condensate back to liquid form.This same principle causes dew in the morning.
If wind blew over a body of water, the thermocline sharpness would likely become less distinct due to the mixing of water layers caused by the wind. The wind would mix the layers, leading to a more gradual transition in temperature between the surface and deeper waters, making the thermocline less defined.
Stratification is defined as the layering of water caused by temperature. I guess you are talking about condensation. Condensation is the transition of gas to liquid, the opposite of boiling.Sometimes it happens that there is a layer of water on objects caused by temperature. This happens when warmer air which contains water in gas from makes contact to a much cooler surface like a cold window or mirror, causing the water to condensate back to liquid form.This same principle causes dew in the morning.
Evaporation is the process in the water cycle that is caused by an increase in temperature. When water temperatures rise, water molecules gain energy and turn into water vapor, which then rises into the atmosphere forming clouds.
evaporation is the energy that release water temperature
The temperature of water typically decreases with depth in the ocean. This is because sunlight penetrates the surface layers, warming them, while deeper layers are colder and more uniform in temperature.
The layers of water typically refer to the different zones within a body of water based on depth and temperature. These layers include the epilimnion (warm, surface layer), thermocline (middle layer with a rapid temperature decrease), and hypolimnion (cold, deep layer). These layers are important for understanding the distribution of organisms and nutrients in aquatic ecosystems.
Thermocline is the term used to describe the layering of water in a body of water due to temperature differences. It is a zone where the temperature changes rapidly with depth.