Sentence examples for cell circulation from inspiring English sources

…Earth's tropical, true desert (BW) climates occur between 15° and 30° latitude, at the poleward end of the Hadley cell circulation (see atmosphere).

Most of Earth's tropical, true desert (BW) climates occur between 15° and 30° latitude, at the poleward end of the Hadley cell circulation (see atmosphere).

At high levels in the atmosphere, the risen air moves away from the equatorial region to descend eventually in the subtropics as it cools; it moves back toward the Equator at low altitudes, completing the Hadley cell circulation pattern.

We will then review the results from studies in living animals that reveal how viruses exploit the natural flow of body fluids, specific tissue architecture, and patterns of cell circulation and migration to spread within the host.

The magnitude of the net meridional winds in Hueso et al. (2012) is below the measurement error and discards strong Hadley cell circulation at this atmospheric altitude in contrast to results in the UV (which sample higher altitudes) where the meridional winds are stronger and the Hadley cell circulation is evident.

In that case, the electrode layer that was formed on the mountain's surface during the night is also diluted after sunrise, and after being transported upslope, the positive charges can be advected over the EFM via the returning cell circulation.

Similar triple-cell circulation patterns were previously earlier found in a number of 3D global simulations models.

The long-time-averaged meridional circulation profile is found to have a three-layer flow structure: an equatorward flow is sandwiched between two poleward flow zones above and beneath it, indicating a double-cell circulation in each hemisphere.

As described above, a two-cell circulation pattern with the dawn cell in counter-clockwise circulation and the dusk cell in clockwise circulation is usually observed by the SuperDARN on the orientation of southward IMF.

Depending on the magnitude of the Ra number and the extent of the flow perturbation, various solutions may be obtained for a bottom-heated enclosure (β = 90°) filled with a pure fluid; these solutions include a single-cell circulation, double-cell horizontal or vertical circulations, clockwise or counterclockwise [6, 35].

Corresponding disturbed reconnection electric fields at a higher latitude magnetopause mapped along the geomagnetic field lines into the polar ionosphere, driving the small sub-cells circulation nested in the cusp.