thermoklineellä
Thermoklineellä is a term used to describe a specific phenomenon related to temperature gradients, particularly in bodies of water. It refers to a layer within a body of water where the temperature changes more rapidly with depth than in the layers above or below it. This transition zone is crucial in understanding the stratification of lakes and oceans.
In most temperate lakes, the thermocline develops during the summer months due to solar heating. The surface
The strength and depth of the thermocline can vary significantly depending on factors such as latitude, wind