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∙ 7y agoThe 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 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
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.
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.
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.
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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.
Ekman upwelling is a process in which winds push surface water offshore, causing deeper, nutrient-rich water to rise to the surface. This upwelling of cold, nutrient-rich water supports high levels of primary productivity and can increase biodiversity in marine ecosystems. It is named after the Swedish oceanographer Vagn Walfrid Ekman who first described this phenomenon.
If the water is cold, that means that water molecules have small speed, in hot water, molecules have greater speed, thus greater energy, and need less energy than cold water to be kicked out through the surface.
An upwelling is a current in the ocean that brings deep, cold water to the ocean surface.