Fort Yukon

General Information

Created: 2014-02-03 08:31:33
Modified: 2014-02-03 08:37:21

Active: No
Country:United States
Site:Fort Yukon
Responsible Countries: United States,
Timezone:UTC/GMT -09:00 hours
Vegetation Type:Forest Tundra
Responsible Person:Leah M. Anderson
Offset:5 m



The town of Fort Yukon is located on the north bank of the Yukon River at its junction with the Porcupine River, about 145 air miles northeast of Fairbanks. It is located 8 miles (13 km) north of the Arctic Circle at the confluence of the Yukon and Porcupine Rivers and in the middle of the Yukon Flats. The 50m2 grid site is ~8 miles (13 km) up the Porcupine River on the South bank (cut-bank).  The Fort Yukon site is imperfectly drained open grassy space surrounded by willows and black spruce.  The ground level slants slightly in towards the middle from all sides, and is wet/marshy through the area.  It is hypothesized to be a potential thermakarst area.  The 50mx50m grid, established in 2009, is marked with survey stakes at 10m intervals.  The NE grid corner (N66.62, W145.62) contains continuous soil temperature & soil moisture sensors at ‘above permafrost’ & ‘just below surface’ levels.  An air temperature sensor also records on a 30 min continuous cycle.  The grid was established in 2009 through a cooperative agreement with Yukon River Inter-Tribal Watershed Council, the U.S. Geological Survey and with assistance from the Council of Athabascan Tribal Government’s Environmental Coordinator and youth from Fort Yukon & Beaver, AK.



The specific location of the Kotlik site was selected using Traditional Ecological Knowledge of permafrost distribution and depth, followed by on-site ground truthing.  

The grid consisted of 50 survey stakes at 10-meter intervals, creating a 50mx50m square grid with a maximum of 100 data points.    Active Layer measurements were taken manually every 5m.  The measurements were taken at the lowest surface level within about 0.3m of the designated point, to minimize the questionable influence of tussocks on the AL measurement.  The "surface level" was determined to be the top of the low-lying vegetation (i.e. moss, lichen, low-bush berries).

[CALM protocol suggests a grid size of 100mx100m, however a 50m2 grid was deemed acceptable due to difficult terrain and length of time for installation (personal communication Dr. V.Romanovsky).]

The soil climate station was established in early September 2009 and is located at the NE grid corner, due to the saturated center and active layer’s greater than 1m. The station monitors air temperature, soil temperature & soil moisture.

The HOBO micro station was installed at the NE grid corner.  A ~30cm4 hole was dug down to the permafrost layer at 75cm. One set of soil moisture and soil temperature sensors were placed just above the permafrost layer (75cm) and one set just below surface level (~10cm).  Soil samples were cut from each level (2x2in cubes) to be analyzed for soil moisture content.

The HOBO pro v2 temp/ext temp sensor was installed, recording air temperature, near the NE grid corner about one meter off the ground surface. The Hobo data logger is set to store data on 30min intervals for up to 428 days. 

GPS points were taken at the four corners of the grid, as well as the center point & where the sensors were located.  Site elevation is 140m, recorded at grid center.

Permafrost Zone:Discontinuous
Vegetation:Grasses, willows, black spruce
Landform:Yukon flats
Lithology:The top 10cm is mossy soil, with the following 65 cm as dense organic soil. The layer just above permafrost had scattered woodchips. The depth to the water table is ~ 1m Black organic Organic layer thickness ~ 65cm
Description:General description of soil moisture : moist
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U48 Fort Yukon

Longitude:-145.1035 °
Latitude:66.62076 °
Elevation:130.65530396 m
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