The movement of deep cold and nutrient-rich water to the surface is known as upwelling. Upwelling occurs when winds push surface water away from a coastline, causing the deep colder water to rise and replace it. This process brings up essential nutrients from the deep ocean to the surface, supporting the growth of phytoplankton and other marine 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.
upwelling
Cold nutrient-rich waters move up to the ocean's surface through a process called upwelling, which occurs when winds push surface water away from the coast, allowing deeper water to rise and replace it. This upwelling brings nutrient-rich waters from the deep ocean to the surface, supporting the growth of phytoplankton and driving the marine food web.
An upwelling occurs when winds push surface water away from the coast, causing cold, nutrient-rich water from the ocean depths to rise to the surface. This process brings essential nutrients to the surface, supporting the growth of phytoplankton and ultimately enhancing marine productivity.
Surface
The movement of deep cold and nutrient-rich water to the surface is known as upwelling. This process occurs when winds blow across the ocean surface, pushing warmer surface waters away and allowing deeper waters to rise. Upwelling is vital for marine ecosystems as it brings nutrients to the surface, supporting the growth of phytoplankton and sustaining diverse marine life.
During upwelling, cold, nutrient-rich water from the deep ocean rises to the surface, often along coastlines. This process typically brings the cold water upward, rather than moving it outward to sea. The upwelled water can then spread horizontally along the surface, supporting marine life, but its primary movement is vertical, from the depths to the surface.
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.
upwelling
Boiling takes place and it leads to the movement of hot water upwards and the movement of cold water downwards.
the movement of deep, cold, nutrient-rich water goes up to the surface. Up-welling can be rising of any liquid. water moving up from the benthic zone
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.
Cold nutrient-rich waters move up to the ocean's surface through a process called upwelling, which occurs when winds push surface water away from the coast, allowing deeper water to rise and replace it. This upwelling brings nutrient-rich waters from the deep ocean to the surface, supporting the growth of phytoplankton and driving the marine food web.
Tropical waters are nutrient poor at the surface. When living things die at the surface they sink to the bottom where they decompose. The nutrients that are released when they decompose stay at the bottom because there's a thermocline--the deep water is cold and the surface water is warm and they don't mix. So the surface waters don't have much algae and stay clearer.
this is one of my favorites questions because my sisters cusins dog always asked this it is idk
An upwelling occurs when winds push surface water away from the coast, causing cold, nutrient-rich water from the ocean depths to rise to the surface. This process brings essential nutrients to the surface, supporting the growth of phytoplankton and ultimately enhancing marine productivity.
An upwelling is a current in the ocean that brings deep, cold water to the ocean surface.