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Using teleseismic body-wave data from the same profile (TIBET-31N), Liang et al. (2016) suggest the asthenosphere upwelling through gaps in the Indian lithosphere and lateral flows above the subducting slab.
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The equatorial cold tongue results from the divergence of surface Ekman currents in response to the large-scale southeast trade winds, which brings cool waters through upwelling into the surface layers.
Tropical cyclones also help maintain the global heat balance by moving warm, moist tropical air to the middle latitudes and polar regions, and by regulating the thermohaline circulation through upwelling.
This fishery could not exist without upwelling.
Upwelling in the open sea has entirely different causes.
Upwelling in coastal waters brings nutrients toward the surface.
Where upwelling occurs, it is responsible for concentrating a profusion of life.
Some of the world's largest fisheries are dependent on upwelling.
The most productive waters of the world are in regions of upwelling.
During the southwest monsoon, upwelling occurs off the Somali and Arabian coasts and south of Java.
According to the upwelling paradigm (Tsunoda, 2015), upwelling growth is produced by the interchange instability with PSSR as the primary driver (see "Upwelling growth model" section).
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