The upwelling of nutrient-rich water along the coast supported a thriving ecosystem of fish and marine life.
Upwelling occurs when strong winds push surface water away from the coast, causing cold, nutrient-rich water from the ocean depths to rise and replace it. This nutrient-rich water supports the growth of phytoplankton and other marine life, making upwelling areas biologically productive.
If an upwelling stops, the nutrient-rich deep waters that are brought to the surface will no longer be available. This can lead to a decrease in primary productivity and a decline in fish populations that rely on these nutrients for food. It can also impact the local climate as upwelling plays a role in ocean circulation patterns.
Upwelling is the process by which cool, nutrient-rich waters from the deep ocean rise to the surface, fueling the growth of phytoplankton and supporting rich marine ecosystems.
upwelling
Upwelling is when the winds cause nutrient rich waters from lower levels of the ocean to replace the surface water. Upwelling's are usually caused by coastal surges or open oceans.
Cold currents near coastlines often indicate the presence of upwelling. This is because upwelling brings cold, nutrient-rich waters from the ocean depths to the surface, leading to colder surface currents. Some examples of cold currents near coastlines that are associated with upwelling include the California Current, the Benguela Current, and the Canary Current.
The two steps of upwelling is
upwelling current upwelling current
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The upwelling of nutrient-rich water along the coast supported a thriving ecosystem of fish and marine life.
Ocean upwelling is a phenomena where cooler deep ocean currents come to the surface, with the usual mechanism being the driving of the water by wind. A more general definition is one that includes the idea of "rising from below or within" as an upwelling of emotion. Here are a couple of sentences: An upwelling of anger fueled his outburst.The thought of the passing of her uncle triggered an upwelling of tears.
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Upwelling is weaker during a normal pattern El Niño event. This is because El Niño brings warmer sea surface temperatures, which suppress the nutrient-rich cold water that drives upwelling along the coast. In contrast, La Niña events typically enhance upwelling due to cooler sea surface temperatures.
Upwelling refers to a rising of seawater, magma, or any other liquid. The upwelling off the California coast is caused by the wind blowing parallel to the coast.
wind
The answer is upwelling.