The phrase "atmosphere circulation" is correct and usable in written English.
It can be used when discussing the movement of air within the Earth's atmosphere, often in the context of meteorology or climate science.
Example: "The study of atmosphere circulation is crucial for understanding weather patterns and climate change."
Alternatives: "air circulation" or "atmospheric circulation".
General fields of research include ocean and atmosphere circulation, ocean-atmosphere interactions, the role of ocean in climate, climate variability and change, paleoclimate.
Possible reasons for the temporal instability of long-term effects of solar activity (SA) and galactic cosmic ray (GCR) variations on the lower atmosphere circulation were studied.
In this work we studied the spatial and temporal structure of long-term effects of solar activity (SA) and galactic cosmic ray (GCR) variations on the lower atmosphere circulation as well as possible reasons for the peculiarities of this structure.
The results obtained provide evidence that the mechanism of solar activity and cosmic ray influences on the lower atmosphere circulation involves changes in the evolution of the stratospheric polar vortex.
We complement this analysis of the middle atmosphere circulation with a classification of both the Arctic and Antarctic winters since 1979 into major, minor, elevated stratopause or quiet winters based on the level of disturbance using the Modern Era-Retrospective Analysis for Research and Applications MERRAA) reanalysis data.
Increases in solar radiation flux effects generally appear at daytime; neutral atmosphere circulation only modulates this process on latitudes.
Introduction to the physics governing the circulation of the atmosphere and ocean and their control on climate with emphasis on the atmospheric circulation.
The freshwater flux couples the ocean to the atmosphere, driving oceanic and atmospheric circulations with impacts on sea surface temperature and salinity6,7.
To take into account the OGW influence on atmospheric dynamics, the above-mentioned parameterization was implemented into the middle and upper atmosphere general circulation model (MUAM) described by Pogoreltsev (2007) and Pogoreltsev et al. (2007).
This phenomenon is robust in observational data and several middle atmosphere general circulation models.
Higher temperatures also lead to more energy entering the atmosphere's circulation that in turn brings more frequent and intense floods, droughts and storms.
