polar cell

The predominant global pattern that affects the climate is the polar cell.

The Polar cell is likewise a simple system.

This vertical cycle comprises the polar cell in each latitudinal hemisphere.

It can be argued that the Polar cell is the primary weathermaker for regions above the middle northern latitudes.

The air in this cell moves according to the differences between moving masses in Hadley and Polar cells.

While the Hadley, Ferrel, and Polar cells are major factors in global heat transport, they do not act alone.

Polar cell may refer to:

There is also a Ferrel cell over the westerlies and a polar cell over the pole.

They are known as the Hadley cell, Ferrel cell, and Polar cell.

By acting as a heat sink, the Polar cell also balances the Hadley cell in the Earth's energy equation.

We recognize 3 cells: the Hadley cell, the Ferrel cell and the Polar cell.

ROT4 and DVL1 are involved in regulating polar cell proliferation on the longitudinal axis of organs.

This process leads to the development of two different populations of cells: Polar cells on the outside and apolar cells on the inside.

In meteorology, the polar front is the boundary between the polar cell and the Ferrel cell in each hemisphere.

The flow breaks up into three separate cells known as the Hadley cell, the Ferrell cell and the Polar cell.

The Arctic front is the semipermanent, semi-continuous weather front between the cold arctic air mass and the warmer air of the polar cell.

In both hemispheres working away from the equator, they are the tropical Hadley cells, the mid-latitude Ferrel, and the polar cells.

In normal epithelial tissues, epithelial cells, or parenchymal cells of epithelia, are highly organized, polar cells.

Polar cells are part of a three-cell movement involving Hadley cells and Ferrel cells which show atmospheric circulation and surface winds.

The wind belts girdling the planet are organised into three cells: the Hadley cell, the Ferrel cell, and the Polar cell.

The earliest specification in mouse embryos occurs between trophoblast and inner cell mass cells in the outer polar cells and the inner apolar cells respectively.

This breaks the hemispheric convection cells into three distinct types of cells: two Hadley cells, two Ferrel cells and two Polar cells.

The Ferrel cell, theorized by William Ferrel (1817-1891), is a secondary circulation feature, dependent for its existence upon the Hadley cell and the Polar cell.

At its southern extent (in the Northern hemisphere), it overrides the Hadley cell, and at its northern extent, it overrides the Polar cell.

This flow is the lower portion of the polar cell, the highest (by latitude) of the three principal circulation cells of the Earth's atmosphere each spanning thirty degrees of latitude.