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- этимология
secondary circulation - перевод на русский
строительное дело
вторичная циркуляция, циркуляция в контуре вторичного теплоносителя
![[[3D rendering]] of a [[high resolution computed tomography]] of the [[thorax]]. The anterior thoracic wall, the airways and the pulmonary vessels anterior to the [[root of the lung]] have been digitally removed in order to visualize the different levels of the pulmonary circulation.](https://commons.wikimedia.org/wiki/Special:FilePath/3D CT of thorax, annotated.jpg?width=200 "[[3D rendering]] of a [[high resolution computed tomography]] of the [[thorax]]. The anterior thoracic wall, the airways and the pulmonary vessels anterior to the [[root of the lung]] have been digitally removed in order to visualize the different levels of the pulmonary circulation.")
![Image showing main pulmonary artery coursing ventrally to the [[aortic root]] and [[trachea]]. The right pulmonary artery passes dorsally to the [[ascending aorta]], while the left pulmonary artery passes ventrally to the [[descending aorta]].](https://commons.wikimedia.org/wiki/Special:FilePath/Relations of the aorta, trachea, esophagus and other heart structures.png?width=200 "Image showing main pulmonary artery coursing ventrally to the [[aortic root]] and [[trachea]]. The right pulmonary artery passes dorsally to the [[ascending aorta]], while the left pulmonary artery passes ventrally to the [[descending aorta]].")
общая лексика
малый [лёгочный] круг кровообращения
медицина
кровообращение в лёгких
лёгочное кровообращение
Определение
Википедия
In fluid dynamics, a secondary circulation or secondary flow is a weak circulation that plays a key maintenance role in sustaining a stronger primary circulation that contains most of the kinetic energy and momentum of a flow. For example, a tropical cyclone's primary winds are tangential (horizontally swirling), but its evolution and maintenance against friction involves an in-up-out secondary circulation flow that is also important to its clouds and rain. On a planetary scale, Earth's winds are mostly east-west or zonal, but that flow is maintained against friction by the Coriolis force acting on a small north-south or meridional secondary circulation.
