Hydrol. Earth Syst. Sci., 24, 1109–1129, 2020 https://doi.org/10.5194/hess-24-1109-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Understanding the relative importance of vertical and horizontal flow in ice-wedge polygons Nathan A. Wales1,2, Jesus D. Gomez-Velez2,3, Brent D. Newman1, Cathy J. Wilson1, Baptiste Dafflon4, Timothy J. Kneafsey4, Florian Soom4, and Stan D. Wullschleger5 1Los Alamos National Laboratory, Los Alamos, NM, 87545, USA 2Hydrology Program, Department of Earth & Environmental Science, New Mexico Institute of Mining and Technology, Socorro, NM, 87801, USA 3Department of Civil and Environmental Engineering, Vanderbilt University, Nashville, TN, 37235, USA 4Earth Science Division, Lawrence Berkeley National Laboratory, Berkeley, CA, 94720, USA 5Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, 37831-6301, USA Correspondence: Nathan A. Wales (
[email protected]) Received: 15 January 2019 – Discussion started: 1 April 2019 Revised: 18 December 2019 – Accepted: 27 January 2020 – Published: 10 March 2020 Abstract. Ice-wedge polygons are common Arctic land- these systems. This work forms a basis for understanding forms. The future of these landforms in a warming climate complexity of flow in polygonal landscapes. depends on the bidirectional feedback between the rate of ice-wedge degradation and changes in hydrological charac- teristics. This work aims to better understand the relative roles of vertical and horizontal water fluxes in the subsurface Copyright statement. The United States Government retains, and of polygonal landscapes, providing new insights and data to the publisher, by accepting this work for publication, acknowledges that the United States Government retains, a nonexclusive, paid-up, test and calibrate hydrological models.