Tundra travel quandary Alaska seeks to protect both North Slope tundra and winter exploration: field work tests just completed, results will be released in November Kristen Nelson Petroleum News Editor-in-Chief
The Alaska Department of Natural Resources is responsible for opening and closing state lands on the North Slope for off-road tundra travel each winter. Since the state began setting a tundra opening date 34 years ago, the window for on-tundra work has shrunk from more than 200 days to around 120.
The department’s Division of Land, Mining and Water has just completed field work testing the tundra impact of different vehicles at different times from fall through early winter. Results are expected in November.
The division is also completing a study on how the tundra opening determination has been made over the years, and evaluating the economic impact of the reduction in the number of days the tundra is open.
Results of the field study will provide scientific data.
It will be, says Harry Bader, the division’s northern region land manager, the first time the state has ever had a scientific basis for its tundra opening decisions. And it’s not an academic exercise. The division has been given a mission, he said: to extend the on-tundra work season while maintaining — or exceeding — the current level of tundra protection.
The number of days allowed for winter tundra work has dropped significantly since the state began to set the tundra opening date in 1969, and a chart of that decline, Bader said Aug. 1, prior to a tour of some of the division’s tundra test plots, has been widely used to illustrate climate change.
And “part of this project is to tease out how much of this graph is a result of climate change and how much is the result of management choice.”
Bader said he hopes to find that a fraction of the changes in the tundra opening dates are due to management choice, “because if it’s entirely climate driven, I’m going to have a hard time opening up the season.” The $1 million study The tundra study is collaborative, Bader said, involving the Department of Natural Resources, the Alaska Oil and Gas Association, the U.S. Department of Energy, Yale University and the University of British Columbia. Costs of the study will come to about $1 million, he said: the Department of Energy provided $270,000 in startup money; the Alaska Oil and Gas Association coordinated personnel and equipment time valued at $80,000; and Yale University computing time is valued at about $700,000.
The division is studying a number of things in what is, Bader said, “the first-ever test on the tundra in a controlled environment.”
One question being asked is “what is the level of disturbance under our current standard?” Public consensus seems to be, he said, that the current level is acceptable. Measuring that level of disturbance is significant, because the division has been asked to change how it opens the tundra so the season will be longer, while maintaining — or enhancing — the present level of tundra protection.
Bader said he wanted people outside the system for the study, and chose to go with academic interns, most of them graduate students, from the University of Alaska Fairbanks, the University of Oregon Law School, McGill University in Canada and Yale University. Two test areas Two test areas were selected, one four miles south of Deadhorse on the coastal plain of the North Slope, and one in the Brooks Range Foothills some 60 miles south of Deadhorse. Selection criteria included: road access; a pullout for staging; no previous activity; and a good representation of the major ecology systems on the North Slope. Given the requirements, there were really only two spots, Bader said, and they weren’t perfect: a helicopter over flight found an old seismic trail — invisible from the ground — at one site, and that “green” trail had to be marked from the helicopter so that the test plots wouldn’t overlay the old disturbance.
The Foothills site is dominated by tussock shrubs, he said, while the coastal plain site is 90 percent wet sedge meadow.
The test work was done over the fall and winter season, and included five treatments on six dates, for a total of 30 plots at each site.
In the treatments vehicles were driven in a figure eight pattern on the plot. The ground was staked to indicate the pattern. Treatments were: a trucker, a wheeled front-end loader, a D-7 cat tractor, a challenger (a rubber-tracked vehicle) and a “no-treatment” treatment.
The “no-treatment treatment” is not the control, Bader said. The control was the baseline ecological data that he and interns working on the project collected the summer before the tests.
The “no-treatment” treatment “is to calibrate the natural variation in change that occurred in the tundra” Bader said. To be significant, any change in the area driven over by, for example, the D-7 Cat, compared to the baseline, “has to be statistically significantly different than the change that occurred in the no-treatment treatments for the same time period.” Measurements crucial to study Baseline ecological data was collected prior to the tests.
Before the driving tests, measurements were made of snow depth, snow slab thickness, hoar frost thickness and ground hardness.
Ground hardness is measured with a drop hammer. One person lifts a weight and drops it; a second person is on the ground, recording how many drops it takes for each inch of penetration by the probe to a depth of 12 inches.
For the vehicle treatments, each was driven over a figure-eight course, marked by stakes.
Bader said the tests, which included 10 passes through the cross “gate” marked by stakes in the center of the figure eight, exceeded anything the division would allow companies to do on the tundra in terms of repeated driving over a single spot.
For each test date, each vehicle was driven in a figure eight pattern on a separate plot; then the plots were left alone. For the next test date, vehicles were driven over different plots.
This enables the division to compare both the date of the test (and the snow and ground hardness conditions on the test date) and the results from different vehicles. October represents “worst case” The test included a late October date, requested by the North Slope Borough to represent a “worst case” scenario. Bader, showing a photo from that test, noted that while there was snow on the ground, the ground was not frozen. “You see a lot of mud and torn-up grass.” While the study results aren’t in yet, he said he doesn’t think October will be an opening date for tundra travel, “because without measuring it, that does look like there’s probably some disturbance.”
This summer Bader and interns Jacynthe Guimond, a graduate of McGill University, in Montreal, Quebec, and University of Alaska Fairbanks undergraduate Jonathan Fiely, returned to the test plots. They took measurements of tussock frequency and disturbance; shrub frequency and disturbance; vegetative cover; depth of active layer; soil temperature at depth; soil volumetric water at depth; and microthermography.
One test, measuring plant stress, used a device developed to measure plant stress on golf courses.
This project will wrap up with modeling, but Yale has applied to the Department of Energy for money to monitor the plots over a 20-year period.
Bader said just entering the data for computer analysis will take 175 to 200 hours.
Has he found a way to increase on-tundra time? Bader says he doesn’t know: look for results in November.
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