The result of diverging surface currents at the geographical equator are the upwelling of cold and also nutrient rich water.
This is known to be the vertical movement of cold and it is one that goes deep and it is said to go into nutrient-rich water to the surface.
The action that causes it is that surface waters tends to move away from area on ocean's surface and this is seen along the equator.
Note also that it often is caused by the divergence of currents along the geographical equator that lead to upwelling of cold, nutrient rich water.
Hence, The result of diverging surface currents at the geographical equator are the upwelling of cold and also nutrient rich water.
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