Understanding the Relative Importance of Vertical and Horizontal Flow in Ice-Wedge Polygons

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 horiz...

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Main Authors: Wales, Nathan A., Gomez-Velez, Jesus D., Newman, Brent D., Wilson, Cathy J., Dafflon, Baptiste, Kneafsey, Timothy J., Wullschleger, Stan D.
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/hess-2019-25
https://www.hydrol-earth-syst-sci-discuss.net/hess-2019-25/
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spelling ftcopernicus:oai:publications.copernicus.org:hessd73991 2023-05-15T15:09:20+02:00 Understanding the Relative Importance of Vertical and Horizontal Flow in Ice-Wedge Polygons Wales, Nathan A. Gomez-Velez, Jesus D. Newman, Brent D. Wilson, Cathy J. Dafflon, Baptiste Kneafsey, Timothy J. Wullschleger, Stan D. 2019-04-01 application/pdf https://doi.org/10.5194/hess-2019-25 https://www.hydrol-earth-syst-sci-discuss.net/hess-2019-25/ eng eng doi:10.5194/hess-2019-25 https://www.hydrol-earth-syst-sci-discuss.net/hess-2019-25/ eISSN: 1607-7938 Text 2019 ftcopernicus https://doi.org/10.5194/hess-2019-25 2019-12-24T09:49:21Z 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 hydrology 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. Samplers 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, then was transported horizontally. Horizontal flow occurred in more locations and at higher velocities of fluxes 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. Text Arctic Copernicus Publications: E-Journals Arctic
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description 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 hydrology 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. Samplers 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, then was transported horizontally. Horizontal flow occurred in more locations and at higher velocities of fluxes 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.
format Text
author Wales, Nathan A.
Gomez-Velez, Jesus D.
Newman, Brent D.
Wilson, Cathy J.
Dafflon, Baptiste
Kneafsey, Timothy J.
Wullschleger, Stan D.
spellingShingle Wales, Nathan A.
Gomez-Velez, Jesus D.
Newman, Brent D.
Wilson, Cathy J.
Dafflon, Baptiste
Kneafsey, Timothy J.
Wullschleger, Stan D.
Understanding the Relative Importance of Vertical and Horizontal Flow in Ice-Wedge Polygons
author_facet Wales, Nathan A.
Gomez-Velez, Jesus D.
Newman, Brent D.
Wilson, Cathy J.
Dafflon, Baptiste
Kneafsey, Timothy J.
Wullschleger, Stan D.
author_sort Wales, Nathan A.
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
publishDate 2019
url https://doi.org/10.5194/hess-2019-25
https://www.hydrol-earth-syst-sci-discuss.net/hess-2019-25/
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source eISSN: 1607-7938
op_relation doi:10.5194/hess-2019-25
https://www.hydrol-earth-syst-sci-discuss.net/hess-2019-25/
op_doi https://doi.org/10.5194/hess-2019-25
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