Category Archives: Science

Humans and Wolves in the Yukon Flats, Alaska

For the last 2.5 years in fulfillment of my Masters in Wildlife Biology at the University of Alaska Fairbanks, I have been researching the biological and human component of two key moose hunters (wolves and humans) within the Yukon Flats. I am happy to say that the full thesis is is completed and that I will be graduating in December! In my eyes, a critical next step is to make the results of this work public. Hence, I will be dedicating four blog entries to the subject. This first installment will introduce  the biology of the region, study area, and my research questions. My next installment will examine access of subsistence hunters to moose within the region. Following that I will look at movement of wolves in the region, and I will conclude by looking at areas were the likelihood of competition between wolves and humans for moose is highest.

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I conducted my research on human hunters and wolves in the Yukon Flats, Alaska. The predator-prey relations in Yukon Flats are unique because wolves and subsistence users pursue low-density moose that are held at a low-density equilibrium from predation. In fact, moose are at some of the lowest densities in the world (<0.20 moose per square kilometer).

Broadly I was interested in:

  1. How do human hunters and wolves utilize their environment when pursuing moose?
  2. How does understanding space use and movement and of humans and wolves pursuing moose help us understand competition for a scarce resource they rely on?

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The Yukon Flats National Wildlife Refuge is located in central Alaska, and extends nearly 220 miles east to west and 120 miles north to south.  It falls directly into a the boreal forest, which means if you walk around that you’ll find birch, black spruce, white spruce, alder and willow. Its namesake is the Yukon River which bisects the Flats, and the huge watershed of the Yukon River is fed by a plethora of rivers. In short, it is a water dominated system.

Yukon Flats
The Yukon Flats National Wildlife Refuge is located north of Fairbanks. It extends nearly 220 miles from east to west and 120 miles north to south.

Yukon Flats

Within the Yukon Flats there are several communities that are defined by their reliance on the land to harvest food, fuel, and fiber. Their subsistence lifestyle provides up to 85% of the resources they use including but not limited to moose, fish, and waterfowl. Since moose are such low densities but are critical for humans and moose,  it is interesting to research how moose are pursued, and where the likelihood of competition between humans and wolves in the highest. Answering any of those questions pertinent for managers.  My thesis integrated spatially explicit (i.e., locations) datasets of moose (Alces alces) hunters and of wolves (Canis lupus) to ultimately evaluate how two predators pursue a common resource, moose.

To this end, Chapter 1 of my thesis will be the second installment on this blog and focus on quantifying rural hunter access in the Yukon Flats, Alaska, through spatially-linked interviews. I chose this research topic because previous studies have only qualitatively surmised use area for subsistence resources by drawing boundaries around use areas. However, a quantitative approach can yield firmer management information. My novel approach provided pertinent insight into resource use for our system and created a method that may be applied to other systems. Using results generated from subsistence hunter interviews, I applied a model of access to moose hunting areas. Harvest reporting is low among the subsistence communities in our study, and from our results we generated an estimate of harvest based on game densities similar to the best data available on reported harvest. As such, my method may provide an alternative to, or supplement, harvest-ticket reporting.

In Chapter 2, I characterized movement paths (i.e., hunt paths) between moose kills by six packs in the Yukon Flats. The results of that work will be the third installment on this blog. The movements of wolves have been studied and documented in many high prey-density systems, but almost no information exists on their movements when prey is just dense (<0.20 /km2) enough for wolves to survive.

Finally, I will tie what I learned about wolf movement and human access to examine where competition between humans is the most likely. At that time, I hope to provide a full copy of the thesis for comprehensive reading of the research. I look forward to sharing this information with you, please feel free to ask questions!

 

 

2016 Alaskan Calendar is Now for Sale!

Hello Everyone,

I am very, very, very  excited to write inform you of the release of my 2016 calendar! The content features some of the best imagery on this website, plus a few things that have never seen the “light of day”. The calendar is entitled “Seasonal Moods of Alaska” with imagery for each month captured in that month. The calendar is 100% designed by me including feature images, transparent images, windows, and text tying the imagery to the season. A huge thanks to my family and fiance for helping to proof the calendar! I believe the final product is a work of art mingled with science.

If you want to see it, clicking on the cover image or link link will bring you to the sales site that I created.  Otherwise, keep reading for some more information 🙂

2016 Seasons and Moods of Alaska Cover

https://ianajohnson.com/customproducts/

The calendar is printed on 9.5×13 paper and spiral bound leaving ample of room to write in your schedule. Of course it has a hole for hanging if that is all you want to do with it! With imagery from throughout Alaska, the calendar is a great memento of your trip to Alaska, for a friend who has been here, or to bring inspiration for your future trip here!

This calendar is being printed by my local shop in Perham, Minnesota. Your consideration and support also helping the local economy in Perham.

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Each month has a premier image. This image from Mendenhall glacier showcases the high resolution imagery within the calendar.
2016 Calendar Final 9halfx1323
Every month has a transparent image behind the grid, and small windows with images from that month. Writing in the lower right panel ties together fuses the imagery and writing together.

The calendar will be available for pre-order through October 15th. At that time I will begin shipping orders. You can help me out a huge amount by spreading the word about this calendar or through a purchase! Thanks you so much in advance for your support in this project!

Watching a Glacier Die

Drop a few ice cubes in your drink before you start reading this, and consider the question : how many licks does it take to get to the center of a Tootsie Pop? Now, while you are thinking about that illusive answer, consider how many days it takes to melt a glacier. Just how fast does it happen? My several trips to Castner Glacier over the last 15 months provide interesting evidence into this impossible to answer question. Let’s take a look!

April 2014

When I first visited Castner Glacier in April 2014 a monstrous, multi-chambered ice cave shook me to my core. The ice cathedral hung over my head an estimated 80 feet above. The walls and ceilings of it were composed of blue, transluscent layers of ice and closer inspection of the walls showed that the clarity of the ice provided a window deep into the glacier of the sediment suspended in it. A chimney was cut into its ceiling allowing light to illuminate the icy floor of the glacier.  It was awe inspiring!

Castner Glacier Face April 2014
This was the glacial face (moraine) as I found it during my April 2014 visit. Clear, blue ice was found in the face, and particularly in the caves.
Castner Ice Cave Cathedral
Once you walked through the ice caves, this cathedral was found on the other side. I guess, based on my height in this picture compared to the ceilings, that the cave was 80 feet tall!
Castner Glacier Chimney
This chimney was found in the ceiling perhaps 20-30 feet above the glacier floor in April 2014. It was very narrow at the top, but the bottom is much wider than this picture would suggest. The icicles at its base suggest that some melting was occurring in it.

This video was taken in April 2014 during a walkthrough of the ice cave and captures the scope of it. Instability of parts of the video was due to the slippery ice floor!

August 2014

The next time I visited the rainiest summer recorded in Fairbanks was coming to a close, and the rain had reshaped the ice in unimaginable ways. Water ran down the glacier in small rivulets and opened the chimney to a yawning mouth. It degraded the ceiling so extremely, that large chunks of the cavern had crashed down. If you stood close to the mouth of the cave many rocks fell dangerously from the ceiling as they melted from their icy tomb of thousands of years. The rapid melt had removed the beautiful transparency from the ice. It was now silty and gray.

Castner Glacier Collapse
When we returned in August 2014 we found the result of the constant rain over the summer. The chimney had melted so rapidly that the roof of the ice cave had collapsed.
Castner Glacier Ice Cave Backside
This image shows the degradation of the chimneys from the top and back of the glacier. Although I didn’t take an April 2014 photo for comparison, this image is especially revealing when compared to June 2015 (upcoming images)
Castner Ice Cave Scale
My parents stand next to the ice cave’s face for perspective. The large blocks that stood in front in April were now gone, and the top of the cave is much, much thinner than just three months earlier. 
Castner Ice Cave Front 2015
This image from the front of the caves shows a large section of ice which caved off the front. The scale and setting of this picture is similar to the April 2014 image of me standing in front of the broad ice cave.

The rapid melting that we witnessed inspired me to create a different type of video for Castner. This video documents the fall (August) stage of plant life around the glacier, and then documents the progression of drops of water from the glacier which eventually build into the silty and fast-flowing Castner Creek.

June 2015

When I visited the Castner Ice Cave in June 2015, it was just a shadow of its former self. Only a small arch of ice remained of the once huge cave. Castner Creek ran through the remnant of the ice cave, where previously it had run to the side. In just fifteen months, unquantifiable amounts of ice from the glacier had transformed into water, carrying with it many tons of silt to the broader river valley that Castner Creek flowed into. The glacier was rapidly changing, dying.

Castner Ice Cave Back June 2015
This image of the Castner Ice Cave was shot in June 2015 from the back. The thin, collapsed chunk of ice in the foreground is all that remains of most of the ceiling of the cave.

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Castner Ice Cave Back Panorama
This image of the back of the Castner Ice Cave can be compared to the images taken in August 2014 and April 2014. The trailing edges of the large ice cathedral that I stood in can be seen in the back right. The arch of the glacier is thin, and a new chimney shows that it continues to degrade.
Castner Glacier Backside Panorama
The trailing edge of the ceiling on the right is all that is left of the ice cathedral from April 2014. Large piles of debris and silt have been deposited, and the floor where the cathedral was is much higher now.

The answer is two hundred fifty-two. At least that is what students at Purdue concluded to the center of a Tootsie Pop. But why does it matter that Alaska’s Castner Glacier and the state’s other glaciers are melting so rapidly? Alaska Dispatch News recently reported on a new study demonstrating that Alaskan Glaciers are losing 75 billion tons (75 gigatons) of ice each year, and that 94% of that loss is occurring on inland glaciers like Castner. This means that Alaskan glaciers will continue to contribute a significant amount to global sea level rise, especially in light of a warming climate. They end the article with a quote by study co-author O’Neel. “This is probably going to be a pretty tough year for a lot of the glaciers”, he stated. It appears he is right, and Castner’s included.