upwelling
Seasonal turnover, also known as lake mixing, is a process where cooler water sinks and replaces warmer water at the surface of a lake. This brings nutrients from the deeper layers to the surface, refreshing the supply of nutrients throughout the lake.
upwelling
No. Think about it. Why do archaeologists usually have to dig down to find the remains of ancient civilizations? The same is true with sedimentary rock history.
Warm surface water and cooler deep water can mix through a process called convection. As warm water cools, it becomes denser and sinks, displacing deeper water and causing mixing. Wind and currents can also help in mixing water layers within a lake.
This process is called lake turnover. During the spring and fall, changes in temperature cause surface water to mix with deeper water layers. This helps distribute nutrients and oxygen throughout the lake, benefiting aquatic life.
Seasonal turnover, also known as lake mixing, is a process where cooler water sinks and replaces warmer water at the surface of a lake. This brings nutrients from the deeper layers to the surface, refreshing the supply of nutrients throughout the lake.
upwhelling
Upwelling.
upwelling
This process is called upwelling. Upwelling occurs when winds push surface water away, allowing cold, nutrient-rich water from deeper levels to rise up to the surface. This phenomenon is important for supporting marine ecosystems by bringing nutrients to the surface and supporting the growth of phytoplankton.
No. Think about it. Why do archaeologists usually have to dig down to find the remains of ancient civilizations? The same is true with sedimentary rock history.
No, typically the layers of rock near the surface are the youngest rocks, as they have been deposited more recently. The deeper layers are usually older as they were deposited earlier in time. This is known as the principle of superposition in geology.
As you go deeper and deeper the layers will start to get hotter and thicker.
Warm surface water and cooler deep water can mix through a process called convection. As warm water cools, it becomes denser and sinks, displacing deeper water and causing mixing. Wind and currents can also help in mixing water layers within a lake.
This process is called lake turnover. During the spring and fall, changes in temperature cause surface water to mix with deeper water layers. This helps distribute nutrients and oxygen throughout the lake, benefiting aquatic life.
The term that describes the rising of cold water from deeper layers to replace warmer surface water is called upwelling. Upwelling occurs when winds push surface water away from the coastline, allowing cold, nutrient-rich water to rise and replace it.
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.