downwelling

How big a sea surface was critical to downwelling?

How much water used to sink in the downwelling?

In the most extreme cases, a lack of downwelling could possibly lead to mass extinction.

The season of warm water movement towards the coast and downwelling for this region is (summer) (winter).

This buildup causes increased pressure on the water column, and leads to downwelling at the front.

This combination will produce downwelling along the land's (eastern) (western) coast.

Another way that downwelling can occur is by the wind driving the sea towards the coastline.

The downwelling has clearly shifted to southwest of Ireland.

His measurements revealed that trenches are sites of downwelling in the solid Earth.

Currents associated with downwelling cycles are slightly stronger than upwelling events.

Cold downwelling material might pond on this transition.

Sea-surface temperatures are relatively high in regions of downwelling.

The downwelling of dense water at the thermal bar acts as a barrier to horizontal mixing.

• Describe the influence of upwelling and downwelling on sea-surface temperatures.

Computer models might not yet be able to predict what will happen if we tamper with downwelling sites, but this problem doesn't seem insoluble.

• Demonstrate the causes of coastal upwelling and downwelling.

Thermal bar formation along the south shore was followed by downwelling throughout the summer, giving a deeper epilimnion.

This downward movement is called downwelling.

Conversely, regions of downwelling transfer carbon (CO) from the atmosphere to the ocean.

A change of air flow of the atmosphere can result in the sinking or downwelling of warm surface water.

Where significant vertical movement of ocean currents is observed, this is known as upwelling and downwelling.

Measurements of downwelling LW at altitude provide the most testing conditions for instrumentation.

However, the temperature of the upwelling is unaffected by downwelling and surface temperature variations.

Features included a substantial fall in thermospheric temperature in the totality region, and a downwelling of the F2 layer.

After downwelling ends, a delamination event within the mantle produces extensional elements of tessera.