- #1
Skyhunter
Here is the abstract.
And here is a related article.
Since we are in the midst of a giant atmospheric experiment, with the only currently habitable planet that we have, I wonder how much understanding the past shifts will help in our understanding of the current climate shift?
The cores suggest that the climate shifts were local, not global like we are seeing today.
And here is a related article.
With the arctic ice melting, should we expect a weakening of the warm northerly flow?As the Antarctic warms, the ocean currents that carry water away from the continent become stronger. Warm water flows as a surface current to the Arctic. Stronger currents transfer more heat to the North Pole, and cool the South. Cold water flows back southward along the ocean floor.
As the Arctic warms, its ice begins to melt. This adds fresh water to the sea, which disrupts the current, because it is less dense than salt water and therefore means that the diluted cold water sinks less readily.
With the current weakened, the Antarctic retains more of the Sun's heat. This warms the southern oceans, eventually causing the there ice to retreat and allowing water to enter the Atlantic from other oceans, thus strengthening the current again and completing the cycle.
Since we are in the midst of a giant atmospheric experiment, with the only currently habitable planet that we have, I wonder how much understanding the past shifts will help in our understanding of the current climate shift?
The cores suggest that the climate shifts were local, not global like we are seeing today.