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The process known as Ekman transport is caused by right-angle winds along a shoreline. The surface water is replaced by deep, colder water from offshore.

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How is wind driven ekman transport related to coastal upwelling and downwelling?

They are both wind driven, if the Ekman Transport is moving in towrds the shore then downwelling will pull water from it and move it down and out. While when the Ekman Transport is moving out away from shore up welling will pull water up and feed the Transport. Note all directions are based on 90 degrees to the left or right fo the wind direction depending on wich Hemisphere.


When is upwelling weaker during a normal pattern El Niño or La Nina event?

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.


What cold currents near coastlines might indicate sites of upwelling?

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.


Which type of flow works in opposition to Ekman transport in a gyre?

Geostrophic flow works in opposition to Ekman transport in a gyre. Geostrophic flow is the balance between the pressure gradient force and the Coriolis force, causing water to move at an angle to the wind direction. This balances the net transport of water caused by Ekman transport.


What does upwelling have to do with el nino?

El Nino reduces upwelling. Normal sea surface temperatures in Pacific tend to be warmer in the west because of upwelling, where warm water flows west because of trade winds and colder water rises up to replace the warm water in the Eastern Pacific. During El Nino, the trade winds get all screwed up and warm water is spread out more evenly in the Pacific. So there is less upwelling and the Eastern Pacific sees warmer sea water.

Related Questions

How is wind driven ekman transport related to coastal upwelling and downwelling?

They are both wind driven, if the Ekman Transport is moving in towrds the shore then downwelling will pull water from it and move it down and out. While when the Ekman Transport is moving out away from shore up welling will pull water up and feed the Transport. Note all directions are based on 90 degrees to the left or right fo the wind direction depending on wich Hemisphere.


Does upwelling happen in open ocean?

Yes, but one type only: equatorial upwelling!There are three types of upwelling: equatorial, coastal, and seasonal.Equatorial upwelling is caused by the winds known as the trade winds. The trade winds blow from east to west in the vicinity of the equator. On the northern side of the equator Ekman Transport is to the right (northward), and on the southern side it is to the left (southward). With water flowing directly away from the equator, both northward and southward, the equator itself has a deficit of water. Hence, water from below upwells to fill in the gap. Equatorial upwelling is most prominent in the Pacific Ocean.


What is the birth name of Hasse Ekman?

Hasse Ekman's birth name is Hans Gsta Ekman.


What is the birth name of Sanna Ekman?

Sanna Ekman's birth name is Maria Susanna Ekman.


What is the birth name of David Ekman?

David Ekman's birth name is David Olof Bertil Ekman.


How tall is David Ekman?

David Ekman is 5' 10".


When was Susanne Ekman born?

Susanne Ekman was born in 1978.


When did Harry Ekman die?

Harry Ekman died in 1999.


When was Harry Ekman born?

Harry Ekman was born in 1923.


When did Ida Ekman die?

Ida Ekman died in 1942.


When was Ida Ekman born?

Ida Ekman was born in 1875.


When did Hilding Ekman die?

Hilding Ekman died in 1966.