Meteorology and snowpack structure associated with avalanche hazard, Porter Heights, Canterbury.

With an increase in use of New Zealand's alpine terrain, there is a growing need to understand processes and phenomena associated with snow avalanche hazard. This research investigates snowpack structure and meteorological influences associated with avalanching at Porter Heights Ski Area and ov...

Full description

Bibliographic Details
Main Author: Allen, Simon Keith
Language:en
Published: University of Canterbury. Department of Geography 2009
Online Access:http://hdl.handle.net/10092/2778
id ndltd-canterbury.ac.nz-oai-ir.canterbury.ac.nz-10092-2778
record_format oai_dc
spelling ndltd-canterbury.ac.nz-oai-ir.canterbury.ac.nz-10092-27782015-03-30T15:30:14ZMeteorology and snowpack structure associated with avalanche hazard, Porter Heights, Canterbury.Allen, Simon KeithWith an increase in use of New Zealand's alpine terrain, there is a growing need to understand processes and phenomena associated with snow avalanche hazard. This research investigates snowpack structure and meteorological influences associated with avalanching at Porter Heights Ski Area and overviews the management practices employed in response to this hazard. Data sources are derived from meteorological and snowpack observations dating back to 1977, coupled with comprehensive field studies in 2003. Weak faceted and mixed crystal forms were found to comprise on average over 40 % of the early season snowpack on sunny and shaded slope aspects, although they could persist on shaded slopes throughout the season, contributing to spring avalanche events. The growth of both lower pack depth hoar, and near-surface facets were strongly influenced by synoptic airflows. Forty-eight hours after the onset of a cool southeast airflow, the temperature gradients in a shallow snowpack ranged from -0.36 °C cm-1 near the surface, to -0.17 °C cm-1 deeper in the pack. A warmer northwest flow induced surface melting, and dramatically altered the thermal regime of the snowpack. Thick layers of rounded grains indicated the importance of equilibrium growth and wind redistribution of snow. Wind loading is most extensive on slopes leeward to the prevalent, strong, west to northwest winds, and slab formation in this terrain is regularly controlled using hand placed explosives and ski cutting techniques. Density measurements centred on a median value of 185 kg/nr' suggested the significance of decomposing new snow in forming surface slabs, with the largest snowfalls at Porter Heights occurring during east to southeast storm events. While this study has cemented a comprehensive understanding of meteorology and snowpack structure at Porter Heights, backcountry avalanche forecasting in the neighbouring terrain will further benefit from larger scale, collaborative future research initiatives.University of Canterbury. Department of Geography2009-09-02T21:19:02Z2009-09-02T21:19:02Z2004Electronic thesis or dissertationTexthttp://hdl.handle.net/10092/2778enNZCUCopyright Simon Keith Allenhttp://library.canterbury.ac.nz/thesis/etheses_copyright.shtml
collection NDLTD
language en
sources NDLTD
description With an increase in use of New Zealand's alpine terrain, there is a growing need to understand processes and phenomena associated with snow avalanche hazard. This research investigates snowpack structure and meteorological influences associated with avalanching at Porter Heights Ski Area and overviews the management practices employed in response to this hazard. Data sources are derived from meteorological and snowpack observations dating back to 1977, coupled with comprehensive field studies in 2003. Weak faceted and mixed crystal forms were found to comprise on average over 40 % of the early season snowpack on sunny and shaded slope aspects, although they could persist on shaded slopes throughout the season, contributing to spring avalanche events. The growth of both lower pack depth hoar, and near-surface facets were strongly influenced by synoptic airflows. Forty-eight hours after the onset of a cool southeast airflow, the temperature gradients in a shallow snowpack ranged from -0.36 °C cm-1 near the surface, to -0.17 °C cm-1 deeper in the pack. A warmer northwest flow induced surface melting, and dramatically altered the thermal regime of the snowpack. Thick layers of rounded grains indicated the importance of equilibrium growth and wind redistribution of snow. Wind loading is most extensive on slopes leeward to the prevalent, strong, west to northwest winds, and slab formation in this terrain is regularly controlled using hand placed explosives and ski cutting techniques. Density measurements centred on a median value of 185 kg/nr' suggested the significance of decomposing new snow in forming surface slabs, with the largest snowfalls at Porter Heights occurring during east to southeast storm events. While this study has cemented a comprehensive understanding of meteorology and snowpack structure at Porter Heights, backcountry avalanche forecasting in the neighbouring terrain will further benefit from larger scale, collaborative future research initiatives.
author Allen, Simon Keith
spellingShingle Allen, Simon Keith
Meteorology and snowpack structure associated with avalanche hazard, Porter Heights, Canterbury.
author_facet Allen, Simon Keith
author_sort Allen, Simon Keith
title Meteorology and snowpack structure associated with avalanche hazard, Porter Heights, Canterbury.
title_short Meteorology and snowpack structure associated with avalanche hazard, Porter Heights, Canterbury.
title_full Meteorology and snowpack structure associated with avalanche hazard, Porter Heights, Canterbury.
title_fullStr Meteorology and snowpack structure associated with avalanche hazard, Porter Heights, Canterbury.
title_full_unstemmed Meteorology and snowpack structure associated with avalanche hazard, Porter Heights, Canterbury.
title_sort meteorology and snowpack structure associated with avalanche hazard, porter heights, canterbury.
publisher University of Canterbury. Department of Geography
publishDate 2009
url http://hdl.handle.net/10092/2778
work_keys_str_mv AT allensimonkeith meteorologyandsnowpackstructureassociatedwithavalanchehazardporterheightscanterbury
_version_ 1716799205023940608