מדאיג: מה קרה לשכבת הקרח בקוטב הצפוני ב-30 השנים האחרונות?
- - - לא מוגה! - - -
In this animation, we're taking art
into the third dimension. Here we're looking at the ice age, which is an indicator of thickness. Generally, older ice is thicker ice. And so, what you see in this animation is first of all the ice pulsing out and in with the seasons. In winter, the ice grows out and expands outward,
and summer it contracts inward as it melts.
In addition, you see the witer ice, which is the older ice,
moving around the Arctic, being pushed around by winds and currents that move the ice. And what you can see is, over the years, the ice pulses around and moves around towards the top along the coast of Greenland, you see that the older ice eventually moves out of the Arctic and into the North Atlantic, where it melts.
But the ice gets replenished within the Arctic because some of the ice survives each summer and grows older.
And particularly in the region north of Alaska called the Bופרט C,
where the ice spins around in a clockwise direction called the Bופרט Jire.
And that ice can keep spinning around,
often times for several years, and gradually getting older and thus getting thicker.
Eventually,
the ice will spin out of that Jire and go out through frם straight.
But in the past,
what has happened, we've always had enough
ice growth and ice aging, enough ice surviving the summers,
to replenish the older ice that's lost.
But in recent years,
we've seen less replenishment.
There's been more melt during the summer,
and so the ice that goes out through frם straight has not been compensated by the ice growth.
In addition,
especially in recent years,
we've seen some pretty remarkable things in the Bופרט Sea,
where that area that used to be a nursery for the development of the older ice,
that allowed the young ice that's allowed to age and mature.
What we've seen instead is the ice is now more broken up,
more scattered,
and that's allowing the older ice to melt within the Bופרט C. So we're seeing the Bופרט C go from a nursery to a graveyard for older ice.
And as we get towards the more recent years,
much of that oldest ice, the ice that's older than five years old,
in the bright white,
has almost virtually disappeared from the Arctic ocean and the Arctic is now dominated by younger and thinner ice.
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