An 11-year record of mass balance of Brewster Glacier, New Zealand, determined using a geostatistical approach
Recognising the scarcity of glacier mass-balance data in the Southern Hemisphere, a mass-balance measurement programme was started at Brewster Glacier in the Southern Alps of New Zealand in 2004. Evolution of the measurement regime over the 11 years of data recorded means there are differences in th...
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Cambridge University Press
2017
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Online Access: | https://doi.org/10.1017/jog.2016.128 https://doaj.org/article/efe5c944cd034ad5ad3b49371c72bd39 |
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ftdoajarticles:oai:doaj.org/article:efe5c944cd034ad5ad3b49371c72bd39 2023-05-15T16:57:32+02:00 An 11-year record of mass balance of Brewster Glacier, New Zealand, determined using a geostatistical approach NICOLAS J. CULLEN BRIAN ANDERSON PASCAL SIRGUEY DOROTHEA STUMM ANDREW MACKINTOSH JONATHAN P. CONWAY HUW J. HORGAN RUZICA DADIC SEAN J. FITZSIMONS ANDREW LORREY 2017-04-01T00:00:00Z https://doi.org/10.1017/jog.2016.128 https://doaj.org/article/efe5c944cd034ad5ad3b49371c72bd39 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143016001283/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.128 0022-1430 1727-5652 https://doaj.org/article/efe5c944cd034ad5ad3b49371c72bd39 Journal of Glaciology, Vol 63, Pp 199-217 (2017) co-kriging geostatistics mass-balance reconstruction mountain glaciers Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.1017/jog.2016.128 2023-03-12T01:30:59Z Recognising the scarcity of glacier mass-balance data in the Southern Hemisphere, a mass-balance measurement programme was started at Brewster Glacier in the Southern Alps of New Zealand in 2004. Evolution of the measurement regime over the 11 years of data recorded means there are differences in the spatial density of data obtained. To ensure the temporal integrity of the dataset a new geostatistical approach is developed to calculate mass balance. Spatial co-variance between elevation and snow depth allows a digital elevation model to be used in a co-kriging approach to develop a snow depth index (SDI). By capturing the observed spatial variability in snow depth, the SDI is a more reliable predictor than elevation and is used to adjust each year of measurements consistently despite variability in sampling spatial density. The SDI also resolves the spatial structure of summer balance better than elevation. Co-kriging is used again to spatially interpolate a derived mean summer balance index using SDI as a co-variate, which yields a spatial predictor for summer balance. The average glacier-wide surface winter, summer and annual balances over the period 2005–15 are 2484, −2586 and −102 mm w.e., respectively, with changes in summer balance explaining most of the variability in annual balance. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Brewster ENVELOPE(169.383,169.383,-72.950,-72.950) New Zealand Journal of Glaciology 63 238 199 217 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
co-kriging geostatistics mass-balance reconstruction mountain glaciers Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
co-kriging geostatistics mass-balance reconstruction mountain glaciers Environmental sciences GE1-350 Meteorology. Climatology QC851-999 NICOLAS J. CULLEN BRIAN ANDERSON PASCAL SIRGUEY DOROTHEA STUMM ANDREW MACKINTOSH JONATHAN P. CONWAY HUW J. HORGAN RUZICA DADIC SEAN J. FITZSIMONS ANDREW LORREY An 11-year record of mass balance of Brewster Glacier, New Zealand, determined using a geostatistical approach |
topic_facet |
co-kriging geostatistics mass-balance reconstruction mountain glaciers Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
Recognising the scarcity of glacier mass-balance data in the Southern Hemisphere, a mass-balance measurement programme was started at Brewster Glacier in the Southern Alps of New Zealand in 2004. Evolution of the measurement regime over the 11 years of data recorded means there are differences in the spatial density of data obtained. To ensure the temporal integrity of the dataset a new geostatistical approach is developed to calculate mass balance. Spatial co-variance between elevation and snow depth allows a digital elevation model to be used in a co-kriging approach to develop a snow depth index (SDI). By capturing the observed spatial variability in snow depth, the SDI is a more reliable predictor than elevation and is used to adjust each year of measurements consistently despite variability in sampling spatial density. The SDI also resolves the spatial structure of summer balance better than elevation. Co-kriging is used again to spatially interpolate a derived mean summer balance index using SDI as a co-variate, which yields a spatial predictor for summer balance. The average glacier-wide surface winter, summer and annual balances over the period 2005–15 are 2484, −2586 and −102 mm w.e., respectively, with changes in summer balance explaining most of the variability in annual balance. |
format |
Article in Journal/Newspaper |
author |
NICOLAS J. CULLEN BRIAN ANDERSON PASCAL SIRGUEY DOROTHEA STUMM ANDREW MACKINTOSH JONATHAN P. CONWAY HUW J. HORGAN RUZICA DADIC SEAN J. FITZSIMONS ANDREW LORREY |
author_facet |
NICOLAS J. CULLEN BRIAN ANDERSON PASCAL SIRGUEY DOROTHEA STUMM ANDREW MACKINTOSH JONATHAN P. CONWAY HUW J. HORGAN RUZICA DADIC SEAN J. FITZSIMONS ANDREW LORREY |
author_sort |
NICOLAS J. CULLEN |
title |
An 11-year record of mass balance of Brewster Glacier, New Zealand, determined using a geostatistical approach |
title_short |
An 11-year record of mass balance of Brewster Glacier, New Zealand, determined using a geostatistical approach |
title_full |
An 11-year record of mass balance of Brewster Glacier, New Zealand, determined using a geostatistical approach |
title_fullStr |
An 11-year record of mass balance of Brewster Glacier, New Zealand, determined using a geostatistical approach |
title_full_unstemmed |
An 11-year record of mass balance of Brewster Glacier, New Zealand, determined using a geostatistical approach |
title_sort |
11-year record of mass balance of brewster glacier, new zealand, determined using a geostatistical approach |
publisher |
Cambridge University Press |
publishDate |
2017 |
url |
https://doi.org/10.1017/jog.2016.128 https://doaj.org/article/efe5c944cd034ad5ad3b49371c72bd39 |
long_lat |
ENVELOPE(169.383,169.383,-72.950,-72.950) |
geographic |
Brewster New Zealand |
geographic_facet |
Brewster New Zealand |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 63, Pp 199-217 (2017) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143016001283/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.128 0022-1430 1727-5652 https://doaj.org/article/efe5c944cd034ad5ad3b49371c72bd39 |
op_doi |
https://doi.org/10.1017/jog.2016.128 |
container_title |
Journal of Glaciology |
container_volume |
63 |
container_issue |
238 |
container_start_page |
199 |
op_container_end_page |
217 |
_version_ |
1766049104664723456 |