Durango
Bill’s
Glaciology
Alaska’s Melting Glaciers
3 examples of retreating glaciers that can be
seen via Alaska’s
26 Glacier Cruise
The most visible aspect of Global Warming is the
shrinkage of Alaska’s glaciers due to rising atmospheric
temperatures. The most obvious way to see that they are melting is
to compare “then and now” aerial photographs of these glaciers.
An easy way to see a large number of Alaska’s
glaciers (before they are gone) is via the “26 Glacier Cruise”.
https://phillipscruises.com/
This cruise can be taken while you are on an ordinary tourist
ocean cruise trip to Alaska.
We will take a brief pictorial visit to 3 of the
tidewater glaciers that can be seen from this cruise trip – the
Harriman, Surprise, and Barry Glaciers that are located in the
western fjords of Prince William Sound. All you have to do to see
these glaciers is sign up for the 26 Glacier Cruise as part of
your Alaskan cruise trip. A bus will pick you up at your ship in
Anchorage, transport you to Whittier, and all you have to do is
walk down the gangplank to your glacier cruise boat.
The map above is from the 26 Glacier Cruise Guide.
The 3 glaciers that we are going to look at (Harriman, Surprise,
and Barry) are north and west of Harriman Fjord.
Harriman Glacier
The Harriman Glacier had been one of Alaska’s few
advancing glaciers up until a few years ago; but now, it too is
beginning to retreat. Tidewater glaciers get their name because
they terminate at sea level in protected fjords. In addition to
ordinary atmospheric melting, the underwater base of a tidewater
glacier is melted by “warm” ocean water. As the underwater base of
a tidewater glacier melts, there is nothing left to support the
above water portion. The collapse of the above-water portion
produces the spectacular “calving events” that are often shown in
Alaskan videos. (For example, see the 2nd video below.)
However, if/when the debris carried by a tidewater
glacier produces a terminal moraine in between the glacier’s
terminal ice front and the ocean; then calving decreases or stops.
The reduction/cessation of oceanic melting will allow some
tidewater glaciers to grow simply because melting decreases faster
than the decrease in snowfall due to global warming. (Please see
http://www.durangobill.com/TakuGlacier/TakuGlacier.html
for a more thorough explanation of this process.)
For awhile, the Harriman Glacier grew because of this
decrease in calving, but recent satellite photographs show that
melting due to Global Warming has overwhelmed even the protection
offered by Harriman’s underwater terminal moraine. The result is
that now, even the Harriman is beginning to shrink.
The picture above is a Google Earth, Sept. 1996 view
of the Harriman Glacier. For photo comparison purposes, draw an
imaginary line from the stream delta near the lower edge of the
photo to a small mud flat near the glacier’s terminus on the
opposite shore.
The above picture (also from Google Earth)
shows the same view but as of May 2012. It appears that the
Harriman Glacier advanced a few hundred feet over the intervening
16 years.
The picture above is a Sept. 30, 2016 Landsat
view of the Harriman Glacier. Glaciers are normally at their most
retreated annual extent during Sept., so this view shows the
Harriman at its most retreated position for the year, but in its
most advanced overall position. A line is drawn from a mountaintop
at the lower right to the edge of a ridge in the upper left.
The picture above is a June 21, 2019 Landsat
view of the Harriman Glacier. Glaciers are normally at their most
advanced annual extent during June., so this view shows the
Harriman at its most advanced position for the year. A line is
drawn from a mountaintop at the lower right to the edge of a ridge
in the upper left.
If you compare the position of the terminus in the
2016 and 2019 views, it can be noted that the Harriman Glacier has
started its retreat during the 3-year period - and the whole
summer melt season is just starting. Note the mud flat (which is
the terminal moraine) that is beginning to appear in front of the
glacier.
The photograph above was taken by the author on
June 10, 2019 and shows the terminus of the Harriman Glacier. The
Harriman Glacier is started to melt back from its most advanced
position - leaving an exposed muddy/silty sandbar that had been
formerly covered with ice. Note that there are no icebergs in the
fjord indicating the face is no longer calving into the ocean.
Surprise Glacier
If you take the 26 Glacier Cruise trip, you will get
up close to the Surprise Glacier. (Not too close because a sudden
calving event of multiple tons of ice might have an “adverse
effect” on the boat’s ability to float. See 2nd video below.)
The picture above is a Google Earth view of the
Surprise Glacier as of Sept. 1996.
Similar to the Harriman Glacier, the Surprise Glacier
advanced slightly from 1996 to 2011.
The picture above is a false color satellite view of
the Surprise Glacier in April 2019. The retreat of the glacier’s
terminus from 2011 is over ½ mile. For example, compare the
glacier vs. the rock fissure just above the 2011 terminus. In the
2019 picture the glacier's terminus is well to the left of the
rock fissure. The Surprise Glacier is now retreating rapidly.
Barry Glacier
The Barry Glacier has been in full retreat
since 1996.
The picture above is a Google Earth view of the Barry
Glacier as of Sept. 1996. The Cascade Glacier enters from the top
left and just joins the Barry for a combined tidewater front. The
Coxe Glacier enters from the lower right edge.
The yellow line superimposed on the Barry Glacier is
Google Earth’s measuring tool. It is used to show how much the
Barry Glacier has retreated.
The picture above is another Google Earth view, but
as of May 2017. Both the Cascade and Coxe Glaciers have retreated
slightly. However, the Barry Glacier has retreated a full 2 miles
in just 21 years. If you could have taken the 26 Glacier Cruise in
1996, the Barry Glacier would have put on a spectacular show with
frequent calving events into the ocean. If you take the same
cruise today, you probably won’t even see the Barry Glacier.
(Assumes no change in the tour route.)
The June 10, 2019 photo above was taken by the author
and shows the retreating face of the Barry Glacier. The Barry
Glacier has retreated 2 miles in the last 21 years.
Similar fates await anyone who postpones a cruise
trip to Alaska. Go see the glaciers as soon as possible. If you
procrastinate for too many years, there won’t be any glaciers left
to see.
Here are 2 of the author’s videos taken from previous
26 Glacier Cruises that include the above glaciers. (The 2nd video
includes a “very very large calving” event of the Surprise
Glacier.)
2014:
https://www.youtube.com/watch?v=q3dGASPPaek&feature=youtu.be
2017:
https://www.youtube.com/watch?v=_nzO_RcrEWw&feature=youtu.be
(Calving at 14:00 into the video)
Also, please see:
The Taku Glacier:
http://www.durangobill.com/TakuGlacier/TakuGlacier.html
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