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current cell - translation to English
![Graph showing a tropical ocean thermocline (depth vs. temperature). <!-- from data collected during the [[International Geophysical Year]]; the data for this plot was collected on 17 May 1957, at roughly 8N, 44W, in the tropical Atlantic. --> Note the rapid change between 100 and 1000 meters. The temperature is nearly constant after 1500 meters depth.](https://commons.wikimedia.org/wiki/Special:FilePath/THERMOCLINE.png?width=200 "Graph showing a tropical ocean thermocline (depth vs. temperature). <!-- from data collected during the [[International Geophysical Year]]; the data for this plot was collected on 17 May 1957, at roughly 8N, 44W, in the tropical Atlantic. --> Note the rapid change between 100 and 1000 meters. The temperature is nearly constant after 1500 meters depth.")
общая лексика
поток воды
течение воды
общая лексика
поверхностный ток
Definition
Wikipedia
The Walker circulation, also known as the Walker cell, is a conceptual model of the air flow in the tropics in the lower atmosphere (troposphere). According to this model, parcels of air follow a closed circulation in the zonal and vertical directions. This circulation, which is roughly consistent with observations, is caused by differences in heat distribution between ocean and land. It was discovered by Gilbert Walker. In addition to motions in the zonal and vertical direction the tropical atmosphere also has considerable motion in the meridional direction as part of, for example, the Hadley Circulation.
The term "Walker circulation" was coined in 1969 by the Norwegian-American meteorologist Jacob Bjerknes.
