From Virginia Tech, a surprising study showing some biological benefit of melting glaciers.
Glacier melt adds ancient edibles to marine buffet

Glaciers along the Gulf of Alaska are enriching stream and near shore marine ecosystems from a surprising source – ancient carbon contained in glacial runoff, researchers from four universities and the U.S. Forest Service report in the December 24, 2009, issue of the journal Nature*.
In spring 2008, Eran Hood, associate professor of hydrology with the Environmental Science Program at the University of Alaska Southeast, set out to measure the nutrients that reach the gulf from five glaciated watersheds he can drive to from his Juneau office. “We don’t currently have much information about how runoff from glaciers may be contributing to productivity in downstream marine ecosystems. This is a particularly critical question given the rate at which glaciers along the Gulf of Alaska are thinning and receding” said Hood.
Hood then asked former graduate school colleague Durelle Scott, now an assistant professor of biological systems engineering at Virginia Tech, to help analyze the organic matter and nutrient (nitrogen and phosphorus) loads being exported from the Juneau-area study watersheds. “Because there are few reports of nutrient yields from glacial watersheds, Eran and I decided to compare the result from a non-glacial watershed with those of a watershed partially covered by a glacier and a watershed fully covered by a glacier,” said Scott.
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Hood and Scott’s initial findings, reported in the September 2008 issue of the journal Nature Geoscience (http://www.nature.com/ngeo/journal/v1/n9/abs/ngeo280.html), presented something of a mystery. As might be expected, there is more organic matter from a forested watershed than from a fully or partially glacier-covered watershed. With soil development, organic matter is transported from the landscape during runoff events. However, there was still a considerable amount of organic carbon exported from the glaciated landscape.
How can a glacier be a source of the organic carbon? His curiosity peeked [sic], in spring 2009, Hood’s Ph.D. student, Jason Fellman, collected samples from 11 watersheds along the Gulf of Alaska from Juneau to the Kenai Peninsula. The samples were analyzed to determine the age, source, and biodegradability of organic matter derived from glacier inputs.
“We found that the more glacier there is in the watershed, the more carbon is bioavailable. And the higher the percentage of glacier coverage, the older the organic material is – up to 4,000 years old,” said Scott.
Hood and Scott hypothesize that forests that lived along the Gulf of Alaska between 2,500 to 7,000 years ago were covered by glaciers, and this organic matter is now coming out. “The organic matter in heavily glaciated watersheds is labile, like sugar. Microorganisms appear to be metabolizing ancient carbon and as the microorganisms die and decompose, biodegradable dissolved organic carbon is being flushed out with the glacier melt,” said Scott.
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How much? “Our findings suggest that runoff from glaciers may be a quantitatively important source of bioavailable organic carbon for coastal ecosystems in the Gulf of Alaska and, as a result, future changes in glacier extent may impact the food webs in this region that support some of the most productive fisheries in the United States,” said Hood.
*The article, “Glaciers as a source of ancient, labile organic matter to the marine environment,” was authored by Hood; Fellman, now at the Institute of Arctic Biology at the University of Alaska Fairbanks; Robert G.M. Spencer and Peter J. Hernes of the Department of Land, Air and Water Resources at the University of California Davis; Rick Edwards and David D’Amore of the Pacific Northwest Research Station of the U.S.D.A. Forest Service in Juneau, and Scott.
The research is supported by Scott and Hood’s three-year grant from National Science Foundation to study the impact of Alaska’s melting glaciers on the transport and fate of nutrients in coastal watersheds in the Gulf of Alaska.
Also as part of the NSF-funded research, this past summer, Scott and his Ph.D. student, Michael Nassry of Hopwood, Pa., along with biological systems engineering senior Andrew Jeffery of Fairfax, Va., who was doing a 10-week undergraduate research study with Hood, conducted the first hydrologic tracer experiment on a supraglacial stream — a stream entirely on top of the glacier. The helicopter company Northstar provided complimentary transportation to the base camp on the Mendenhall Glacier, where the team injected a salt, reactive nitrogen, and phosphorus over a 150 meter range, then collected water samples over a five-hour period. “At the end of the experiment, the helicopters were no longer flying, which provided the opportunity to sleep on top of the glacier,” said Scott. Samples from this experiment are still being analyzed, and initial findings will be presented at the annual meeting of the American Geophysical Union December 14-18 in San Francisco.
Learn more about Eran Hood’s research at http://www.uas.alaska.edu/dir/ewhood.html
Learn more about Durelle Scott’s research at https://filebox.vt.edu/users/dscott/web/


Peeked or piqued? Clearly the way AW handled it with (sic) is proper, since he is quoting the source.
As for word choice, I would suggest “aroused” rather than picqued. Since my Websters define piqued as: to arouse resentment in, as by slighting as its first definition.
After reading a number of scientific papers, press releases and blog postings on climate change, may I suggest that we follow Hemingway’s example, and write so the reader, doesn’t have to stop and use a dictionary and or a text book to understand what the writer is trying to say. Maybe requiring the first $20 of every grant be spent on a copy of Strunk & White’s The Elements Of Style.
Three points : First this is a short term upside if it proves to be a finding that can be extended to other glaciers. The retreat of the Juneau Icefield system is extensive.
http://glacierchange.wordpress.com/2009/11/01/215/
http://www.nichols.edu/departments/Glacier/juneau icefield.htm
Second glaciers can have considerable biologic activity that losses in area do not help. http://www.nichols.edu/departments/Glacier/iceworm.htm
Third there have been lots of dye tracer experiments in supraglacial streams, I did some on the Juneau Icefield even in the early 1980’s. And have annually used these in the North Cascades since 1984
Hi,
I just wanted to alert Watts up With That readers to a farmer in Australia who is on hunger strike. The Australian Government has stolen his property rights (Carbon Credits) to meet their Kyoto targets. Kevin Rudd ponced around Copenhagen, with targets met. On the backs of all Australian farmers.
Can I encourage others to click on the link below, and add their comments to the Daily Telegraph story?
http://www.dailytelegraph.com.au/news/dying-for-a-chat-with-kevin-rudd/comments-e6freuy9-1225814235842
pat (15:35:46) :
When I went to Glacier Bay, we were accompanied by a Federal Ranger who was an American Indian from the area. He told a fascinating ‘legend’ of how his people once inhabited the area but years of unrelenting snow caused the fjord or deep bay to become glaciated. Archeologist and cartographers have since confirmed the bay was much more ice free in historical times.
maybe the most valuable comment on this whole thread.
It has often amazed me how the glacial studies of Alaska parallel findings in the Alps. As some glaciers receded in recent years in the alps, the glaciers were exposing wood of about the same age, with the average being about 5500 years. During the Holocene optimum some 5 to 7 thousand years ago, many of the alpine passes that are now glaciated were ice free and forested.
Sea levels were also about 2 meters higher than they are today. There was also another significant climate shift about 2000 years ago, when climate started cooling as it has since on a millennial scale.
Yes, to read the MSM and listen to Mr. Gore you might think the ice will soon be gone, but of course they don’t want real scientists to venture forth and find the truth about nature.
Ha! I shared some office space with Scotty when he spent some time at MIT in the late 1990’s. Great guy.
John F. Hultquist (16:08:17) :
“Has anyone mentioned soot?”
Yeah, haven’t you heard of the soot chewing arctic snapper?
Since the first glacier formed so many millions of years ago, they have been melting, even during Ice Ages. What’s the big deal? I guess another benefit of global warming hysteria is that the nature is glacial runoff is being studied.
peeked? peeked? peeked? Is this what a college education gets you these days? I can understand a misspelling/typo in a quickie comment; those quickies are messy affairs – the comments, that is. But when a formal statement/press release is posted by a higher education institution, I would expect a bit more due diligence in proofing before unveiling that short bit of prose to the entire world’s scrutiny.
And, veering a bit OT, to the weather*. Here in Buffalo, today’s forecast was terribly wrong. … Again. The snow that was supposed to miss me – didn’t.
This morning’s weather showed the patch of overnight snow clearing the area with a forecast (advisory) of lake effect snows well to the south of here. Figured I’d head out in the afternoon and make quick work of the two or three inches in an hour or so. … Right. Except that I ended up being parked right in the center of the target. And they changed the forecast several times this afternoon to issue lake effect snow warnings – after it kicked in. Looks like we got another ½’ of snow by the time the sun set and the lake effect snows finally drifted to the south where they were supposed to be all day – according to the ealier forecast. And now the wind’s picking up, which will make tomorrow’s shoveling even more fun through all that drifting snow and frigid temps (10-15°F) and strong winds.
*[You know that it’s weather when you can see that the model {forecast} turns out to be wrong. Climate is when the model {forecast} can’t be proven wrong because, when the predicted event occurs, you are likely to already be dead, so the climate forecast is safe. Besides, there will also be newer, more robust models in place, so the failure of a previous model is irrelevant.]
Well, thank God all that extra carbon is being eaten. What would happen if it all went to CO2???
Is the Gaia Hypothesis biting the biter? Rather than nasty humans destroying her with their evil carbon, she merely activates previously unsuspected mechanisms to turn the situation in her favor and prosper.
A delicious idea to savor.
Oh yeah.
/sarc
DirkH (16:01:34) :
No they won’t:
Hey, that may be what WE want to believe, but didn’t Dr.Al say they’d be gone by 2035 or thereabouts? Start you freshman year now, go for your doctorate, you might not even have your loans paid off before it’s time for a new job in a different field, likely with some more education.
And how is someone and their life partner(s) going to take care of their replacement units then? Think about the unactivated economic productivity providers!
WEll we shouldn’t be making fun of the paper, even of its spellings.. But whether or not this is a good discovery; I doubt that it relates in any meaningful way to climate. We’ll find out eventually if this is important in some way; other than getting more grants for the researchers.
Whoops, that should have been “start your freshman year.”
This site has no comment edit function, and I am avoiding complaining about other people’s spelling. 🙂
This pictures says so much.
http://3.bp.blogspot.com/_ynOO15XuGnc/SyeybHWFxGI/AAAAAAAACJQ/xI2SNbhQ4hY/s1600-h/Alaskan_tree_stump_glacier.jpg
Drought is what is causing glaciers in Glacier Nat’l Park to recede, not temperature.
http://www.nrmsc.usgs.gov/files/norock/products/Pederson-et-al_EI_2006.pdf
Terrific Glacier Page.
http://www.appinsys.com/GlobalWarming/GW_4CE_Glaciers.htm
Big report on Himalayan Glaciers, melting since 1850 like the rest.
http://climaterealists.com/index.php?id=4392
Speaking of Alaska, the temperature change occurred in 2 yrs and have since stabilized.
http://climate.gi.alaska.edu/ClimTrends/Change/TempChange.html
Seems to be on the downswing.
http://climate.gi.alaska.edu/ClimTrends/Change/7708Change.html
They’ve just rediscovered the Holocene Optimum.
John K. Sutherland (14:54:56) said:
In a fit of pique the author clearly misspelled “piqued.”
[1]pique
1 /pik/ pronunciation [peek], piqued, piqu⋅ing, noun
–verb (used with object)
1. to affect with sharp irritation and resentment, esp. by some wound to pride: She was greatly piqued when they refused her invitation.
2. to wound (the pride, vanity, etc.).
3. to excite (interest, curiosity, etc.): Her curiosity was piqued by the gossip.
4. to arouse an emotion or provoke to action: to pique someone to answer a challenge.
5. Archaic. to pride (oneself) (usually fol. by on or upon).
–verb (used without object)
6. to arouse pique in someone: an action that piqued when it was meant to soothe.
–noun
7. a feeling of irritation or resentment, as from a wound to pride or self-esteem: to be in a pique.
8. Obsolete. a state of irritated feeling between persons.
Origin:
1525–35; < MF pique (n.), piquer (v.) < VL *piccare to pick 1 ; see pickax, pike 2 , piqué
And sorry, i have to say the WWF has completely missed out on the threat to the ice worm:
http://deadlinescotland.wordpress.com/2009/12/29/2403/
No, this report is utterly wrong. There will be mass extinctions, destruction, and death. DOOM I say! DOOM!
Oh rats, the font size tag didn’t work. Anyway, I forgot to say that the curiosity is thus:
Alaskan glaciers have organic matter in them, but weren’t we told they are leftovers from the last glacial maximum? So, 2.5 to 4 thousand years ago, there was no ice in Alaska? Why is that? Where was the runaway tipping point? Where were the positive feedback cycles that kept Alaska from freezing over? Hmmm?
“Drought is what is causing glaciers in Glacier Nat’l Park to recede, not temperature.”
That study only goes to 2000. I haven’t been able to find much newer than 2002. Anyone have any idea what the glaciers have been doing the past couple of years?
The whole point of “unequivocal” and “the science is settled”, of course, is to abort the debate and silence the science.
DirkH (15:45:59) :
Don’t worry.
Sorry, but the linked article doesn’t help. [And I had to refresh myself on the power prefixes to know that PgC was Peta (10 ^ 15) grams of Carbon.] It clearly says most of the theoretically available carbon is stored in the deep ocean. The sedimentation processes lead to carbon sequestering for millions of years. It takes quite a long time for the geological processes to make what was ocean bottom into surface land, where weathering and biological activity can reduce the rock to where the carbonates can be converted to usable carbon forms. Waiting for tectonic action, for plates to subduct so the sedimentary rocks get melted and the carbon released, is likewise going to take awhile.
In the meantime, evolution has provided us with plants that are highly efficient at wringing the available carbon from their environment. And the sedimentation continues. Plus, cold water can hold more CO2. If we did enter an ice age, how quickly would the oceans soak up the atmospheric CO2? It could be a rather sudden downward trend, and since we are starting with such low atmospheric levels to begin with, we could bottom out at plant death relatively quickly. Cutting carbon emissions may be cutting down a buffer zone we will dearly need later.
“kadaka (18:05:37) :
[…]
Cutting carbon emissions may be cutting down a buffer zone we will dearly need later.”
Now i see your point. You’re right about that. The orthodoxy would call us lunatics to fear the opposite of what they fear. I’ve just been on von Storch’s blog, he started one, it’s called klimazwiebel which is german for climate onion. Nothing much to see there, he has a poll running about whether people like a “how to debunk denier’s arguments” page he links to. He’s so nineties (back then when global warming was a scare).
One thing to keep in mind is that because a glacier is retreating at its face does not mean that it is not accumulating mass overall. It can take a hundred years or more for increased accumulation at high altitude to flow down and be seen at the termination of the glacier. 2007 and 2008 saw years were there were several feet of snow left from the previous season when the new snows of the current season arrived. It looks like 2010 will be another such year if current snowfall totals hold up. And, interestingly enough, this is reflected in both Alaska and the Italian Alps. In 2008 there was still snow at sea level in Valdez in June.
In many cases what is happening at the face of the glacier is an indication of what has happened over the past 50 years or more and might not be an indication of what is happening overall at the current time. Drought conditions 100 years ago might manifest today as glacial retreat even though the upper reaches of the glacier might be gaining mass today.