Understanding the relative importance of vertical and horizontal flow in ice-wedge polygons

<p>Ice-wedge polygons are common Arctic landforms. The future of these landforms in a warming climate depends on the bidirectional feedback between the rate of ice-wedge degradation and changes in hydrological characteristics. This work aims to better understand the relative roles of vertical...

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Main Authors: N. A. Wales, J. D. Gomez-Velez, B. D. Newman, C. J. Wilson, B. Dafflon, T. J. Kneafsey, F. Soom, S. D. Wullschleger
Format: Article
Language:English
Published: Copernicus Publications 2020-03-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/24/1109/2020/hess-24-1109-2020.pdf
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spelling doaj-a50852b7ed054111b7b8622ed2ef04452020-11-25T01:20:05ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382020-03-01241109112910.5194/hess-24-1109-2020Understanding the relative importance of vertical and horizontal flow in ice-wedge polygonsN. A. Wales0N. A. Wales1J. D. Gomez-Velez2J. D. Gomez-Velez3B. D. Newman4C. J. Wilson5B. Dafflon6T. J. Kneafsey7F. Soom8S. D. Wullschleger9Los Alamos National Laboratory, Los Alamos, NM, 87545, USAHydrology Program, Department of Earth & Environmental Science, New Mexico Institute of Mining and Technology, Socorro, NM, 87801, USAHydrology Program, Department of Earth & Environmental Science, New Mexico Institute of Mining and Technology, Socorro, NM, 87801, USADepartment of Civil and Environmental Engineering, Vanderbilt University, Nashville, TN, 37235, USALos Alamos National Laboratory, Los Alamos, NM, 87545, USALos Alamos National Laboratory, Los Alamos, NM, 87545, USAEarth Science Division, Lawrence Berkeley National Laboratory, Berkeley, CA, 94720, USAEarth Science Division, Lawrence Berkeley National Laboratory, Berkeley, CA, 94720, USAEarth Science Division, Lawrence Berkeley National Laboratory, Berkeley, CA, 94720, USAEnvironmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, 37831-6301, USA<p>Ice-wedge polygons are common Arctic landforms. The future of these landforms in a warming climate depends on the bidirectional feedback between the rate of ice-wedge degradation and changes in hydrological characteristics. This work aims to better understand the relative roles of vertical and horizontal water fluxes in the subsurface of polygonal landscapes, providing new insights and data to test and calibrate hydrological models. Field-scale investigations were conducted at an intensively instrumented location on the Barrow Environmental Observatory (BEO) near Utqiaġvik, AK, USA. Using a conservative tracer, we examined controls of microtopography and the frost table on subsurface flow and transport within a low-centered and a high-centered polygon. Bromide tracer was applied at both polygons in July 2015 and transport was monitored through two thaw seasons. Sampler arrays placed in polygon centers, rims, and troughs were used to monitor tracer concentrations. In both polygons, the tracer first infiltrated vertically until encountering the frost table and was then transported horizontally. Horizontal flow occurred in more locations and at higher velocities in the low-centered polygon than in the high-centered polygon. Preferential flow, influenced by frost table topography, was significant between polygon centers and troughs. Estimates of horizontal hydraulic conductivity were within the range of previous estimates of vertical conductivity, highlighting the importance of horizontal flow in these systems. This work forms a basis for understanding complexity of flow in polygonal landscapes.</p>https://www.hydrol-earth-syst-sci.net/24/1109/2020/hess-24-1109-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author N. A. Wales
N. A. Wales
J. D. Gomez-Velez
J. D. Gomez-Velez
B. D. Newman
C. J. Wilson
B. Dafflon
T. J. Kneafsey
F. Soom
S. D. Wullschleger
spellingShingle N. A. Wales
N. A. Wales
J. D. Gomez-Velez
J. D. Gomez-Velez
B. D. Newman
C. J. Wilson
B. Dafflon
T. J. Kneafsey
F. Soom
S. D. Wullschleger
Understanding the relative importance of vertical and horizontal flow in ice-wedge polygons
Hydrology and Earth System Sciences
author_facet N. A. Wales
N. A. Wales
J. D. Gomez-Velez
J. D. Gomez-Velez
B. D. Newman
C. J. Wilson
B. Dafflon
T. J. Kneafsey
F. Soom
S. D. Wullschleger
author_sort N. A. Wales
title Understanding the relative importance of vertical and horizontal flow in ice-wedge polygons
title_short Understanding the relative importance of vertical and horizontal flow in ice-wedge polygons
title_full Understanding the relative importance of vertical and horizontal flow in ice-wedge polygons
title_fullStr Understanding the relative importance of vertical and horizontal flow in ice-wedge polygons
title_full_unstemmed Understanding the relative importance of vertical and horizontal flow in ice-wedge polygons
title_sort understanding the relative importance of vertical and horizontal flow in ice-wedge polygons
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2020-03-01
description <p>Ice-wedge polygons are common Arctic landforms. The future of these landforms in a warming climate depends on the bidirectional feedback between the rate of ice-wedge degradation and changes in hydrological characteristics. This work aims to better understand the relative roles of vertical and horizontal water fluxes in the subsurface of polygonal landscapes, providing new insights and data to test and calibrate hydrological models. Field-scale investigations were conducted at an intensively instrumented location on the Barrow Environmental Observatory (BEO) near Utqiaġvik, AK, USA. Using a conservative tracer, we examined controls of microtopography and the frost table on subsurface flow and transport within a low-centered and a high-centered polygon. Bromide tracer was applied at both polygons in July 2015 and transport was monitored through two thaw seasons. Sampler arrays placed in polygon centers, rims, and troughs were used to monitor tracer concentrations. In both polygons, the tracer first infiltrated vertically until encountering the frost table and was then transported horizontally. Horizontal flow occurred in more locations and at higher velocities in the low-centered polygon than in the high-centered polygon. Preferential flow, influenced by frost table topography, was significant between polygon centers and troughs. Estimates of horizontal hydraulic conductivity were within the range of previous estimates of vertical conductivity, highlighting the importance of horizontal flow in these systems. This work forms a basis for understanding complexity of flow in polygonal landscapes.</p>
url https://www.hydrol-earth-syst-sci.net/24/1109/2020/hess-24-1109-2020.pdf
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