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'latitudinal circulation' is a correct and usable phrase in written English.
This phrase typically refers to the movement of air masses between different latitudes. For example, "The latitudinal circulation of the atmosphere influences global climate patterns."
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The average temperature of the earth surface, the convective conductance in the horizontal direction as well as other parameters defining the latitudinal circulation also match the observed values.
It has certainly favoured "latitudinal" circulation (precisely circulation along the geomorphological features) of human and animal populations despite the global climatic changes.
Earth's atmosphere includes six latitudinal circulation zones, three in each hemisphere.
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This period also witnessed the closure of the Tethys sea when the African plate collided with the Eurasian one (c. 18-17 Myr), bringing an end to the moist influence of the latitudinal oceanic circulation system [ 15, 69].
They are, in essence, a three-celled latitudinal arrangement of the atmospheric circulation, with the systems in the Northern and Southern hemispheres mirroring each other on opposite sides of the Equator.
We interpret the observed spatiotemporal deposition patterns to latitudinal shifts of the tropical easterly circulation in the early to mid-Holocene and the temperate westerly circulation in the late Holocene.
Gravity wave transports of momentum, heat, energy, and minor constituents have a strong effect on background variations of the upper mesosphere and lower thermosphere (MLT), including the seasonal-latitudinal variations of the general circulation.
Jupiter has no solid surface hence, no topographic features and the planet's large-scale circulation is dominated by latitudinal currents.
The Indian Ocean can be subdivided into four general latitudinal climatic zones based on atmospheric circulation: monsoon, trade winds, subtropical and temperate, and subantarctic and Antarctic.
The three-dimensional pattern of winds over the Earth, known as general circulation, is responsible for the fundamental latitudinal structure of pressure and air movement and, hence, of climates.
Changes in global atmospheric circulation during the Miocene-Pleistocene led to a latitudinal shift of the South Westerlies towards the Equator.
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