Geometric Evolution of Polygonal Terrain Networks in the Canadian High Arctic: Evidence of Increasing Regularity over Time

Polygon networks are usually described qualitatively as becoming more regular through time, but such a concept has yet to be demonstrated numerically. The aim of this study is to address this question quantitatively in order to determine if polygonal terrain networks actually become more regular as...

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Published in:Permafrost and Periglacial Processes
Main Authors: Timothy W. Haltigin, Wayne H. Pollard, Pierre Dutilleul, Gordon R. Osinski
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://doi.org/10.1002/ppp.1741
id ftrepec:oai:RePEc:wly:perpro:v:23:y:2012:i:3:p:178-186
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spelling ftrepec:oai:RePEc:wly:perpro:v:23:y:2012:i:3:p:178-186 2023-05-15T13:58:36+02:00 Geometric Evolution of Polygonal Terrain Networks in the Canadian High Arctic: Evidence of Increasing Regularity over Time Timothy W. Haltigin Wayne H. Pollard Pierre Dutilleul Gordon R. Osinski https://doi.org/10.1002/ppp.1741 unknown https://doi.org/10.1002/ppp.1741 article ftrepec https://doi.org/10.1002/ppp.1741 2020-12-04T13:31:25Z Polygon networks are usually described qualitatively as becoming more regular through time, but such a concept has yet to be demonstrated numerically. The aim of this study is to address this question quantitatively in order to determine if polygonal terrain networks actually become more regular as they develop. Spatial point pattern analysis (SPPA), which can quantify overall network geometries based on the randomness or regularity exhibited by the spatial arrangement of polygon‐bounding trough intersections, was used at three ice‐wedge polygon sites in the Canadian High Arctic. SPPA was applied in two ways: (i) on the present‐day networks observed in the field; and (ii) on historical arrangements derived by distinguishing primary from secondary troughs. In all cases, the polygonal networks had undergone a statistically significant regularisation over the course of their development. Although the method was applied only to terrestrial ice‐wedge polygons, such an approach may also be useful for interpreting the evolution of Antarctic sublimation polygons and geometrically similar polygonal networks on Mars. Copyright © 2012 John Wiley & Sons, Ltd. and Her Majesty the Queen in Right of Canada. Article in Journal/Newspaper Antarc* Antarctic Arctic RePEc (Research Papers in Economics) Arctic Antarctic Canada Permafrost and Periglacial Processes 23 3 178 186
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Polygon networks are usually described qualitatively as becoming more regular through time, but such a concept has yet to be demonstrated numerically. The aim of this study is to address this question quantitatively in order to determine if polygonal terrain networks actually become more regular as they develop. Spatial point pattern analysis (SPPA), which can quantify overall network geometries based on the randomness or regularity exhibited by the spatial arrangement of polygon‐bounding trough intersections, was used at three ice‐wedge polygon sites in the Canadian High Arctic. SPPA was applied in two ways: (i) on the present‐day networks observed in the field; and (ii) on historical arrangements derived by distinguishing primary from secondary troughs. In all cases, the polygonal networks had undergone a statistically significant regularisation over the course of their development. Although the method was applied only to terrestrial ice‐wedge polygons, such an approach may also be useful for interpreting the evolution of Antarctic sublimation polygons and geometrically similar polygonal networks on Mars. Copyright © 2012 John Wiley & Sons, Ltd. and Her Majesty the Queen in Right of Canada.
format Article in Journal/Newspaper
author Timothy W. Haltigin
Wayne H. Pollard
Pierre Dutilleul
Gordon R. Osinski
spellingShingle Timothy W. Haltigin
Wayne H. Pollard
Pierre Dutilleul
Gordon R. Osinski
Geometric Evolution of Polygonal Terrain Networks in the Canadian High Arctic: Evidence of Increasing Regularity over Time
author_facet Timothy W. Haltigin
Wayne H. Pollard
Pierre Dutilleul
Gordon R. Osinski
author_sort Timothy W. Haltigin
title Geometric Evolution of Polygonal Terrain Networks in the Canadian High Arctic: Evidence of Increasing Regularity over Time
title_short Geometric Evolution of Polygonal Terrain Networks in the Canadian High Arctic: Evidence of Increasing Regularity over Time
title_full Geometric Evolution of Polygonal Terrain Networks in the Canadian High Arctic: Evidence of Increasing Regularity over Time
title_fullStr Geometric Evolution of Polygonal Terrain Networks in the Canadian High Arctic: Evidence of Increasing Regularity over Time
title_full_unstemmed Geometric Evolution of Polygonal Terrain Networks in the Canadian High Arctic: Evidence of Increasing Regularity over Time
title_sort geometric evolution of polygonal terrain networks in the canadian high arctic: evidence of increasing regularity over time
url https://doi.org/10.1002/ppp.1741
geographic Arctic
Antarctic
Canada
geographic_facet Arctic
Antarctic
Canada
genre Antarc*
Antarctic
Arctic
genre_facet Antarc*
Antarctic
Arctic
op_relation https://doi.org/10.1002/ppp.1741
op_doi https://doi.org/10.1002/ppp.1741
container_title Permafrost and Periglacial Processes
container_volume 23
container_issue 3
container_start_page 178
op_container_end_page 186
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