Alaska
& Global warming |
Don
Bertolette |
Mar
09, 2006 20:45 PST |
Roman-
Probably appropriate of nothing, I thought back ten years to a
summer spent
in the A, B, C islands in SE Alaska...we were looking to
establish inventory
plots every 4.4 kilometers, and one particular one fell, in the
context of a
topographic map base (dated in the early 1960s, like many AK
topos are), on
a glacier. We then tried to view this location with satellite
imagery, but
(because of the difficulty of getting cloud free imagery in
Alaska in
general, and particularly in regions with glaciers) we weren't
able get
satisfactory imagery. Several months later, we visited the plot
location,
just then beginning to revegetate with pioneering species, the
glacier
having receded hundreds of meters. In less than forty years.
This was about the same time that the spruce bark beetle
population was
exploding on the Kenai Peninsula, as Ed Holsten said, due to
unusually warm
winters, that weren't cold enough to keep the beetle in check.
During the last two months spent in Alaska, it was clear from
multiple
sources, that Alaskan researchers view the last 50 years as
significantly
out of hrov, nrov, and many other rov...
-Don
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There are some out of the ordinary warming events as
well. For instance,
peat cores in AK that show a history of 10,000 years
have no woody
material until the last 50 or so years. In other words
this is a major
warming event for teh last 10,00 years.
And remember peat preserves very, very well.
Roman Dial
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RE:
Global warming story on public radio |
Roman
Dial |
Mar
12, 2006 19:00 PST |
Don,
We are straying from eastern native trees a bit here but there
are many
topo mpas that indicate where glacial ice used to be. I was just
driving back from central Alaska (where I lived from 1977 to
1988)
yesterday when I looked up and recalled a glacier in a cirque
that was
there in the early eighties and is now gone.
However, the most dramatic example I have seen personally was a
3 square
mile icefield/glacier that covered a 5000 foot peak in the
Alaska Range
in the 1950's and by the late 80's was gone -- completely gone.
Indeed
using Google Earth I just looked at the site and all the ice is
gone.
Just one tiny little patch of snow at the summit. I visited the
site in
1989 and it was cryptogamic and moss covered soil.
We also had a bad outbreak of spruce bark beetles round here
(Anchorage)
and on the Kenai Peninsula. A colleague of mine, Ed Berg,
ecologist with
Kenai National Wildlife Refuge says that one reason the beetles
got so
out of control is that long, hot summers allowed the beetles to
finish
their life cycle in one year rather than two, effectively
doubling their
intrinsic rate of increase. Additionally, the trees that seemed
to be
most susceptible were hybrids between white spruce and Sitka
spruce.
Sitka spruce can only grow where the precip is sufficient, and
maybe
they are able to "weep" the penetrating female beetles
out as they try
to get in and lay eggs. Perhaps the white spruce grow where it
is simply
too cold for the beetles to overwinter. And where it's not too
cold and
not too wet, that's where the hybrid trees are and the beetles
hit a
startling number of trees over a certian size class (like about
10
inches DBH).
The Kenai Peninsula has no permafrost and no domestic grazing
animals
and relatively small areas of human develoment. Yet it has
substantially
drying wetlands, rising tree line, shrinking glaciers, and
expanding
shrubs, all of which are unprecedented, there, at least, and
over the
last 50 years it is clearly visible..
Roman
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