PERMAFROST GROWN
  • Home
  • Art and Science Walk
    • 1 Introduction Panel
    • 2 Finding Our Way Around Permafrost
    • 3 What Is Permafrost
    • 4 Types Of Permafrost
    • 5 The Active Layer
    • 6 The Farm Beneath Our Feet
    • 7 Mulch Zucchini
    • 8 People and Permafrost Grain
    • 9 Permafrost Drilling and Coring
    • 10 Ice Wedges In Fields
    • 11 Mapping Using Remote Sensing
    • 12 Polygons Of New Knowledge
    • 13 Canopy Collapse Thaw Crack
    • 14 Rings On The Move
    • 15 Drunken Trees Rings
    • 16 Story Of Slimtree Farm
    • 17 Movement Of Knowledge
    • 18 Credits
  • Meet the Team
    • UAF Researchers
    • Collaborating Farms
  • Methods
  • Near Real-time Data
    • Goldstream Valley
    • Farmers Loop
    • CHSR
    • UAF Farm
    • Anaktuvuk Pass
  • Publications and Media
  • Background Information
    • Permafrost in Alaska
    • Agriculture in Alaska
  • Contact Us

Permafrost Grown Art & Science Walk

Click here to view a pdf version of the original panel format. 

Mapping using remote sensing

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A colorized point cloud showing trees, walking trail and a lake in an area of the Bicycle Bumps Walking Trail on UAF campus.
A digital surface model of the ground surface underlying the trees in the image above. The surface terrain shows the bumpy topography created by melting ice wedges. A faint line approximately located on the center-right side is the Bicycle Bumps Walking Trail.
Remote sensing is a science that uses images taken from satellites, airplanes and drones to create maps and identify landscape changes over time.

Permafrost Grown uses a remote sensing method called Light Detection and Ranging (LiDAR).

LiDAR emits laser pulses that bounce off objects, allowing us to create three-dimensional maps of the canopy and ground surface, such as these maps on
the left of UAF’s bicycle bumps walking trail.

This field was cleared for cultivation in 1908, but in 1918 thaw subsidence caused by melting ice wedges created the mounds or “bumps.” After repeated grading attempts and reappearing mounds, the field was abandoned in the 1920s.

While the forest has grown back, the mounds remain.
Photos taken from an airplane from 1951, 1984 and 2007 show the expansion of a farm field in Fairbanks, Alaska.
Three images from 1951, 1984 and 2007 of the same farm showing farm field expansion overtime. There is a black outline in all images that shows the final dimension of the field in 2007 to help compare the field size in the other time steps.
C​omparing 2011 and 2017 LiDAR datasets, we measured up to 1.05 meters (3.4 feet) of subsidence and made the map on the right.

Notice that thaw subsidence does not occur everywhere in the field; this is because ground ice content in permafrost can be highly variable.
This image shows the amount of thaw subsidence (ground surface collapse) that was measured between 2007 and 2017 using digital terrain models at the same farm field in the time series above. The highest amount of thaw subsidence is up to 1.05 meters (3.4 feet) and it is generally present on the left side and corresponds to the last areas that were cleared for field expansion.
References:
A version of the farm expanding time series and subsidence measurement figure above is published in:
Ward Jones, M., Habeck, O.H., Ulrich, M., Crate, S., Gannon, G., Schwoerer, T., Jones, B., Kanevskiy, M., Baral, P., Maharjan, A., Steiner, J., Spring, A., Price, M.J., Bysouth, D., Forbes, B.C., Verdonen, M., Kumpula, T., Strauss, J., Windirsch, T., Poeplau, C., Shur, Y., Gaglioti, B., Parlato, N., Tao, F., Turetsky, M., Grand, S., Unc, A., and Borchard, N. (2024). Socio-ecological dynamics of diverse global permafrost-agroecosystems under environmental change. Arctic, Antarctic, and Alpine Research, 56(1). https://doi.org/10.1080/15230430.2024.2356067. 

The 2011 and 2017 LiDAR datasets used in the figure references above was provided by:
 Alaska Division of Geological and Geophysical Survey Staff. 2013. Elevation datasets of Alaska: Alaska division of geological & geophysical surveys digital data series 4, https://elevation.alaska.gov/
Research led by Benjamin Jones, associate research professor at the Institute of Northern Engineering and a co-investigator on the Permafrost Grown Project.
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  • Home
  • Art and Science Walk
    • 1 Introduction Panel
    • 2 Finding Our Way Around Permafrost
    • 3 What Is Permafrost
    • 4 Types Of Permafrost
    • 5 The Active Layer
    • 6 The Farm Beneath Our Feet
    • 7 Mulch Zucchini
    • 8 People and Permafrost Grain
    • 9 Permafrost Drilling and Coring
    • 10 Ice Wedges In Fields
    • 11 Mapping Using Remote Sensing
    • 12 Polygons Of New Knowledge
    • 13 Canopy Collapse Thaw Crack
    • 14 Rings On The Move
    • 15 Drunken Trees Rings
    • 16 Story Of Slimtree Farm
    • 17 Movement Of Knowledge
    • 18 Credits
  • Meet the Team
    • UAF Researchers
    • Collaborating Farms
  • Methods
  • Near Real-time Data
    • Goldstream Valley
    • Farmers Loop
    • CHSR
    • UAF Farm
    • Anaktuvuk Pass
  • Publications and Media
  • Background Information
    • Permafrost in Alaska
    • Agriculture in Alaska
  • Contact Us