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Betty Pingo MNT

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General Information

Created: 2014-02-03 14:19:22
Modified: 2015-11-09 16:11:02

Active: No
Country:United States
Site:Betty Pingo
CALM-Code:U7 B
Responsible Countries: United States,
Timezone:UTC/GMT -09:00 hours
Vegetation Type:Tundra
Responsible Person:Nikolay Shiklomanov
Type:Grid
Nodes:0
Rows:
Columns:
Offset: m

DESCRIPTION OF AREA CONTAINING SITE:

U7B 1-ha grid is located within of the U7A 1 km grid.

Site description: Flat with mixed flat-centered and low-centered polygons; moist nonacidic tundra.

Vegetation communities: (1) Raised microsites, including polygon rims and raised centers: Moist Eriophorum triste, Carex membranacea, Dryas integrifolia, Tornentypnurn nitens, Thamnolia subuliformis graminoid, prostrate-shrub tundra. (2) Lower microsites, mainly polygon basins: Wet Eriophorum angustifolium, Carex aquatilis, Drepanocladus brevifolius graminoid tundra.Cover of top 5 species: Eriophorum triste (22%), Dryas integrifolia (16%), Tomentypnum nitens (7%), Eriophorum vaginatum (4%), Carex aquatilis (2%).

 Mean vegetation height: 3.1 +/- 3.0 s.d. cm

Mean live moss layer thickness: 1.8 +/- 0.9 cm

Organic layer thickness: 12 +/- 1.7  cm.

 (Walker and Bockheim, 1995)

 

SAMPLING DESIGN AND METHOD:

Beginning in 1995, the active layer has been probed at least annually at the site. The procedure involves pushing a metal rod, calibrated in cm, to the point of refusal, interpreted in most cases to be the frost table. Thaw depth measurements at each site were obtained by probing at 5 m intervals along the plot’s two perpendicular and one diagonal transect, resulting in 71 points per plot per probing date.

 

In 1995 the site was instrumented with several OnsetTM portable data loggers connected to probe-type thermistors. Each logger/thermistor system has an effective temperature range of -50oC to +33oC and resolution of approximately 0.32oC. At each site, one thermistor was placed in a radiation shield approximately 2 m above the ground surface, and nine loggers were placed at the interface between mineral soil and organic material in various microtopographic positions within the site. Temperature measurements were collected at, 1 hr, and 2 hr intervals depending on season, and year. Details on methodology are provided in Klene et. al 2001.

This soil climate station was established in June of 1996 and is located on the British Petroleum (BP) Prudhoe Bay oil field near Betty pingo within U7a and U7b CALM sites. The elevation is about 12 m (40 ft). This station monitors air temperature, soil temperature at various depths to a maximum of 120 cm, and soil water content at 10, 25, and 40 cm depths. Measurements are made at 20-minute intervals and averaged and recorded every hour.

 

DATA

Soil temperature and soil moisture metadata and data are also available at http://soils.usda.gov/survey/scan/alaska/BettyPingo/

Additional Climate data are also available at http://www.uaf.edu/water/projects/NorthSlope/coastal_plain/betty/betty.html

Aspect:149
Permafrost Zone:Continuous
Vegetation:Flat with mixed flat-centered and low-centered polygons; moist nonacidic tundra
Landform:Outer coastal plain, drained lake basins
Lithology:Pergelic Cryoborolls (55%), P. Cryaquolls (16%), P. Cryaquepts (16%), others (13%). Organic layer thickness: 12 +/- 1.7cm mineral texture -- silty loam /silt/peat
Access Timeseries
Bibliographic References
Klene A.E., Nelson F.E., and N.I. Shiklomanov. 2001 The n-factor as a tool in geocryological mapping: seasonal thaw in the Kuparuk River Basin, Alaska. Physical Geography, 22(6): 449-466.
http://dx.doi.org/10.1080/02723646.2001.10642754
Walker, D. A., and J. G. Bockheim, Site selection for the portable flux towers, ARCSS/LAII/Flux Study, 1316 June 1995, Summary of field activities, Land-Atmos.-Ice Interact. Sci. Manage. Off., Geophys. Inst.,Univ. of Alaska-Fairbanks, 1995.
http://dx.doi.org/10.2172/290848
Shiklomanov, N.I. and F.E. Nelson. 2003 Climatic variability in the Kuparuk region, north-central Alaska: optimizating spatial and temporal interpolation in a sparse observation network. Arctic, 56: 136-146.
http://dx.doi.org/10.14430/arctic609
Shiklomanov, N.I. and F.E. Nelson. 2003 Statistical representation of landscape-specific active-layer variability. In Phillips, M., Springman, S. M., and Arenson, L. U. (eds.), Proceedings of the Eighth International Conference on Permafrost, vol. 2. Lisse: A.A. Balkema, 1039-1044.
http://dx.doi.org/10.1016/b978-0-444-53643-3.00095-9
Walker D.A., Jia G.J., Epstein H.E., Raynolds M.K., Chapin III F.S., Copass C., Hinzman L.D., Kane D., Knudson J.A., Maier H., Michaelson G.J., Nelson F.E., Ping C.L., Shiklomanov N.I., Romanovsky V.E., Shur Y. 2003 Vegetation-soil-thaw-depth relationships along a Low Arctic bioclimatic gradient, Alaska: Synthesis of information from the Atlas studies. Permafrost and Periglacial Processes, 14: 103-123.
http://dx.doi.org/10.1002/ppp.452
Shiklomanov N. I. and F. E. Nelson, F. E., 2002. Active-layer mapping at regional scales: a 13-year spatial time series for the Kuparuk region, north-central Alaska. Permafrost and Periglacial Processes, 13: 219-230.
http://dx.doi.org/10.1002/ppp.425
Klene A.E., Nelson F.E., Shiklomanov N.I., and K.M. Hinkel. 2001 The n-factor in natural landscapes: Variability of air and soil-surface temperatures, Kuparuk River basin, Alaska. Arctic, Antarctic and Alpine Research, 33(2): 140-148.
http://dx.doi.org/10.1080/15230430.2001.12003416
Nelson, F.E., Shiklomanov, N.I., and G.R. Mueller. Variability of active-layer thickness at multiple spatial scales, north-central Alaska, USA. 1999 Arctic, Antarctic, and Alpine Research, 31(2): 179-186.
http://dx.doi.org/10.2307/1552606
Bockheim, J.G., Walker, D.A., Everett, L.R., Nelson, F.E. and N.I. Shiklomanov. 1998 . Soils and cryoturbation in moist nonacidic and acidic tundra in the Kuparuk River basin, Arctic Alaska, USA. Arctic and Alpine Research, 30(2): 166-174.
http://dx.doi.org/10.2307/1552131
Nelson, F.E., Hinkel, K.M., Shiklomanov, N.I., Mueller, G.R., Miller, L.L., and D.A. Walker. Active-layer thickness in north central Alaska: systematic sampling, scale, and spatial autocorrelation. 1998 Journal of Geophysical Research-Atmospheres, 103(D22): 28963-28973.
http://dx.doi.org/10.1029/98jd00534
Nelson, F.E., Outcalt, S.I., Brown, J., Shiklomanov, N.I., and K.M. Hinkel. Spatial and temporal attributes of the active-layer thickness record, Barrow, Alaska, USA, 1998 Proceedings of the Seventh International Conference on Permafrost. Centre de etudes nordiques de l'Universite Laval, Laval, Quebec, Canada, Yellowknife, NWT, Canada, pp. 797-802
http://dx.doi.org/10.1002/ppp.3430010210
Walker, D.A., Auerbach, N.A., Bockheim, J.G., Chapin, F.S., Eugster, W., King, J.Y., McFadden, J.P., Michaelson, G.J., Nelson, F.E., Oechel, W.C., Ping, C.L., Reeburg, W.S., Regli, S., Shiklomanov, N.I., and G.L. Vourlitis.1998 Energy and trace-gas fluxes across a soil pH boundary in the arctic. Nature, 394(6692): 469-472.
http://dx.doi.org/10.1038/28839
Nelson F.E., Shiklomanov, N.I., Mueller G.R., Hinkel K.M., Walker D.A., and J.G. Bockheim.1997 Estimating active-layer thickness over a large region: Kuparuk River basin, Alaska, USA. Arctic and Alpine Research, 29(4): 167-378.
http://dx.doi.org/10.2307/1551985
Shiklomanov, N.I. and F.E. Nelson. Analytic representation of the active layer thickness field, Kuparuk River basin, Alaska. 1999 Ecological Modelling, 123: 105-125.
http://dx.doi.org/10.1016/s0304-3800(99)00127-1

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Longitude:-148.8928 °
Latitude:70.2835 °
Elevation:8 m
EPSG:4326
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