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===Description=== | ===Description=== | ||
Stratification refers to the layering of water with different physical and chemical properties. Large bodies of water are stratified into distinct layers, with each an unique composition. The vertical layering is determined by factors such as salinity, density, and temperature. | Stratification refers to the layering of water with different physical and chemical properties. Large bodies of water are stratified into distinct layers, with each an unique composition. The vertical layering is determined by factors such as salinity, density, and temperature. | ||
Generally speaking there are multiple different types of layers, starting at the top: | Stratification has important implications for marine biology, ocean circulation, and the distribution of nutrients and gases. Generally speaking there are multiple different types of layers, starting at the top: | ||
# Epipelagic Zone, which refers to the surface layer, generally warmer and less dense than the other layers. This layer is usually well-mixed due to wind, wave and current action, and extents from the top to a few hundred meters below. | # Epipelagic Zone, which refers to the surface layer, generally warmer and less dense than the other layers. This layer is usually well-mixed due to wind, wave and current action, and extents from the top to a few hundred meters below. |
Revision as of 13:02, 19 December 2023
This page was last edited on 19 December 2023, at 13:02. Content is available under GPLv3 unless otherwise noted.