temperature stratification

**Temperature Stratification**

Temperature stratification refers to the layering of water or air at different temperatures, typically occurring in natural bodies of water such as lakes, oceans, or reservoirs. This phenomenon results in distinct thermal layers, where warmer, less dense water sits above cooler, denser water. Temperature stratification can significantly impact aquatic ecosystems, water quality, and mixing processes. It is an important concept in environmental science, meteorology, and hydrology, influencing everything from seasonal turnover in lakes to thermal pollution in water bodies.