It's called membrane potential.
No.
The convection cell that lies to the north of the polar jet stream is called the Polar Cell. This cell is characterized by cold air descending near the poles and moving toward the equator at the surface, creating a circulation pattern that influences weather patterns in polar regions. The Polar Cell operates alongside the Ferrel Cell and the Hadley Cell, contributing to the overall atmospheric circulation.
Phospholipids :)
they have a polar head and non-polar tails
The Ferrell cell sits between the polar cell and Hadley cell. It is fueled by atmospheric circulation patterns that transport air between the two cells. Air moves poleward from the Hadley cell and equatorward from the polar cell, interacting within the Ferrell cell to form a complex system of atmospheric circulation.
subpolar low
The three major convection cells in the atmosphere are the Hadley cell, Ferrel cell, and Polar cell. The Hadley cell is near the equator, the Ferrel cell is mid-latitude, and the Polar cell is near the poles. These cells are responsible for redistributing heat and moisture around the globe.
The Polar cell lies to the north of the Polar jet stream in the atmosphere. This cell is characterized by cool air sinking at the poles, moving towards lower latitudes at the surface, and then rising at around 60° latitude to complete the circulation loop.
During oogenesis, the polar body is a small cell that is formed as a byproduct when the egg cell divides. The polar body typically does not have the ability to develop into a mature egg cell and eventually disintegrates.
It would dissolve in water or in polar liquids and would not be recognisable as a cell.
Yes, polar molecules can cross the cell membrane through facilitated diffusion or active transport.
The convection cell that lies to the north of the polar jet stream is the polar cell. This cell is one of the three major atmospheric circulation cells and is characterized by cold air descending at the poles, flowing towards the equator at the surface, and rising again at around 60 degrees latitude. The polar jet stream, which is a fast-flowing air current, forms at the boundary between the polar cell and the mid-latitude Ferrel cell.