Subsurface Flow Across Polygonal Tundra Measured by Bromide Tracer, Utqiagvik (Barrow), Alaska, 2015-2016

DOI: https://doi.org/10.5440/1342954
NGEE Arctic Record ID: NGA130
Data Version: 1.0
Abstract

A bromide tracer study with the primary focus on hydrology in the active layer of polygonal tundra in the Barrow Environmental Observatory in Utqiagvik (Barrow), Alaska from July 2015 to September 2016. Sampling devices placed at various depths in the polygon centers, rims, and troughs were used to monitor tracer concentrations during thaw seasons. The tracer was continually monitored simultaneously on a low- and high-centered polygon throughout thaw seasons. Included is one data file of the bromide tracer concentrations. Also included are measurements taken throughout the experiment - one data file each of frost table depth and precipitation; and twelve water table elevation data files. Water level data, meteorological data, and thaw depth measurements were taken throughout the experiment. Our approach permits a comparison of hydrological behaviors in low- and high-centered polygons over the same time period and meteorological conditions.

The Next-Generation Ecosystem Experiments: Arctic (NGEE Arctic), was a 10-year research effort (2012-2022) to reduce uncertainty in Earth System Models by developing a predictive understanding of carbon-rich Arctic ecosystems and feedbacks to climate. NGEE Arctic was supported by the Department of Energy's Office of Biological and Environmental Research.

The NGEE Arctic project had two field research sites: 1) located within the Arctic polygonal tundra coastal region on the Barrow Environmental Observatory (BEO) and the North Slope near Utqiagvik (Barrow), Alaska and 2) multiple areas on the discontinuous permafrost region of the Seward Peninsula north of Nome, Alaska.

Through observations, experiments, and synthesis with existing datasets, NGEE Arctic provided an enhanced knowledge base for multi-scale modeling and contributed to improved process representation at global pan-Arctic scales within the Department of Energy's Earth system Model (the Energy Exascale Earth System Model, or E3SM), and specifically within the E3SM Land Model component (ELM).

Authors
Nathan Wales (nwales@lanl.gov) 0000-0003-2442-7431
Brent Newman (bnewman@lanl.gov) 0000-0001-9177-8675
Cathy Wilson (cjw@lanl.gov) 0000-0001-9896-0912
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Dataset Citation
Nathan Wales, Brent Newman, Cathy Wilson. 2020. Subsurface Flow Across Polygonal Tundra Measured by Bromide Tracer, Utqiagvik (Barrow), Alaska, 2015-2016. Next Generation Ecosystem Experiments Arctic Data Collection, Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tennessee, USA. Dataset accessed on [INSERT_DATE] at https://doi.org/10.5440/1342954.
Dates
2015-07-03 - 2016-09-30
Geographic Location
NGEE Arctic Utqiagvik (Barrow), Alaska
North71.35
South71.2
East-156.4
West-156.7
Place Keywords:
Barrow, Alaska | North Slope, Alaska | Barrow Environmental Observatory | Utqiagvik, Alaska
Subject Keywords:
geochemistry | bromide concentration | frozen ground | depth | precipitation | hourly precipitation | ground water | water table depth |
GCMD Keywords
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > GROUND WATER
EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > WATER QUALITY/WATER CHEMISTRY
EARTH SCIENCE > LAND SURFACE > FROZEN GROUND
EARTH SCIENCE > ATMOSPHERE > PRECIPITATION
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Methodology
One high-center polygon and one low-center polygon were chosen to reflect the extremes of tundra polygon morphology. Each polygon was instrumented with six fully-screened observation wells, one in the center of the polygon and five distributed along the surrounding troughs. Pressure transducers were deployed in each well to measure stage fluctuations at fifteen-minute intervals and used to estimate water table elevations relative to ground surface. Precipitation was measured using a tipping gauge rain bucket, 65 m from the study site. MacroRhizon samplers (Rhizosphere Research Products, Netherlands) were used to sample pore water at various locations and depths in both study sites. These samplers minimize perturbations to the porous media matrix and flow field by collecting sample volumes at low rates, no greater than 60 ml day-1, driven by the suction of a syringe at the surface. Sample depths refer to the insertion depth of sampler tip ends. The rims of each polygon had 8 nests of MacroRhizon samplers oriented in a radial pattern around the polygon. Each sampler nest had samplers at 3 depths: 15 cm, 25 cm, and at the frost table. Samplers at the 15- and 25-cm depths were fixed over time while the deepest sampler, installed once the frost table reached a depth of 35 cm, was moved downward on a weekly basis as the frost table depth increased. Troughs surrounding each polygon also had 8 nests of samplers adjacent to corresponding sampler nests on the rims. Three nests of samplers were placed in the center of the low-center polygon and only one in the center of the high-center polygon due to its smaller relative area. Samples were frozen and shipped to the Geochemistry and Geomaterials Research Laboratory at Los Alamos National Laboratory for analysis. Samples were thawed and filtered through a 0.45-µm syringe filter prior to analysis via ion chromatography with an uncertainty of +/-5%. For more information on the Materials and Methods, see Wales, 2020. Some of the precipitation data used in this dataset (Hinzman, 2014) include values of 6999.00 which is an invalid precipitation measurement and likely caused by instrument malfunction. Data were gap-filled for 6999.00 value with NOAACRN data for Barrow, AK.
Related References
Wales, N. A., Gomez-Velez, J. D., Newman, B. D., Wilson, C. J., Dafflon, B., Kneafsey, T. J., Soom, F., and Wullschleger, S. D.: Understanding the Relative Importance of Vertical and Horizontal Flow in Ice-Wedge Polygons, Hydrol. Earth Syst. Sci., 24, 1109-1129, 2020, https://doi.org/10.5194/hess-24-1-2020
Related Identifiers
Type: DOI
Relation: IsCitedBy
Type: DOI
Relation: IsCompiledBy
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Metadata Contact
Contact information for the individual or organization that is knowledgeable about the data.
Person: Nathan Wales
Organization: Los Alamos National Laboratory
Email: nwales@lanl.gov
Point of Contact
Contact information for the individual or organization that is knowledgeable about the data.
Person: Brent Newman
Email: bnewman@lanl.gov
Dataset Usage Rights
Public Datasets

This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this license, visit https://creativecommons.org/licenses/by/4.0.

See the NGEE Arctic Data Policies for more details https://ngee-arctic.ornl.gov/data-policies.

Distribution Point of Contact
Contact: Data Center Support
Organization: Next-Generation Ecosystem Experiments (NGEE) Arctic Project, Oak Ridge National Laboratory
Email: support@ngee-arctic.ornl.gov