Arctic
Methane: Why The Sea Ice Matters
Interviews
with:
James
Hansen - NASA
Natalia
Shakhova - IARC
Peter
Wadhams - Cambridge University, UK
David
Wasdell - Apollo-Gaia Project
http://envisionation.co.uk/
James
Hansen:
If it begins to allow the Arctic Ocean to warm up and warm the ocean
floor, then we'll begin to release methane [from] hydrates, and if we
let that happen, that's a potential tipping points that we don't want
to pass. There are now observations that methane is beginning to
be released by both melting tundra on the land and bubbling up in the
Arctic Ocean, indicating some warming of the Arctic Ocean.
Natalia
Shakhova:
The total amount of methane in the current atmosphere is about 5 Gt.
The amount of carbon preserved in the form of methane in the East
Siberian Arctic Shelf is ~ from hundreds to thousands Gt. What
divides this methane from the atmosphere is a very shallow water
column and a weakening permafrost, which is losing its ability to
serve as a seal. This area is very seismically and tectonically
active and there was some investigation that the tectonic activity is
increasing.
Peter
Wadhams:
At the rate we're going, it will bring us to an ice-free Arctic in
about four years time. [The Arctic Ocean] now warms up to about
5 degrees [5oC
or 41oF,
i.e.] enough to start warming up the seabed. The seabed at the moment
is frozen, but it's now starting to melt. That's allowing a lot of
methane which is trapped under the permafrost to be released. That's
a large boost to global warming, because methane is an extremely
powerful climatically-active gas.
David
Wasdell:
The warm water from the surface is now being mixed down to those
areas that it never reached when the whole area was covered in sea
ice. As soon as the area is open water, you have a process of heating
that goes right down to those clathrate deposits on the seabed. The
more the methane is released into the atmosphere, the faster the
heating goes. It's probably the greatest threat we face, as a planet.
We're already in a mass extinction event.
- From 2 years ago (2010)
- From 2 years ago (2010)
No comments:
Post a Comment
Note: only a member of this blog may post a comment.