3. De mondiale transportband

Inleiding

The ocean helps shape climate around the world. Ocean currents transport heat from equator towards the poles, releasing heat to the atmosphere along the way. Warm currents also release moisture to the air, and influence regional rainfall patterns.

Chapter 2 looked at the surface currents. In this chapter we look at the vertical circulation.

Vertical circulation is driven by cold, salty water sinking at high latitudes and returning towards the equator in the deep ocean. This water is replaced by warm water moving towards to poles at the surface.

This vertical overturning acts like a conveyor belt, transporting heat from the tropics to high latitudes. It is the subject of this chapter.

North Atlantic sea surface temperature from satellites for January 2008.

Why is the Arctic port of Murmansk ice free all year?

Murmansk in the Arctic (top) and the Baltic ports near St. Petersburg (bottom) are both important for Russian access to the Atlantic. Despite St. Petersburg being much further south, it is surrounded by ice for a month or more each year, while Murmansk is always ice free.