Finally, Larry sent a great picture of our team standing
atop a large permafrost degradation feature in Barrow. This area was the result
of a disturbance several years ago, but it illustrates nicely the processes we
are trying to study. On one hand, low-centered polygons represent healthy
permafrost conditions; we saw many of these this week. On the other hand,
degraded areas can form where permafrost has warmed. This warming can result in
thawing of the permafrost and subsequently set up strong interactions with
surface hydrology. Thermal erosion can quickly, in a matter of a few years to a
decade, drive the formation of these degradation features. As you can see there
is considerable subsidence in these areas, the soil dries, and you can get
rapid mortality of tundra vegetation. Our NGEE Arctic project wants to
understand the natural processes that might also lead to these "features
of the future" and represent them in models. We believe this to be a major
step towards better understanding critical landscape-scale feedbacks to climate
in the Arctic.
Cheers...