Variability in glacier albedo and links to annual mass balance for the gardens of Eden and Allah, Southern Alps, New Zealand
The gardens of Eden and Allah (GoEA) are two of New Zealand's largest ice fields. However, their remote location and protected conservation status have limited access and complicated monitoring and research efforts. To improve our understanding of the spatial and temporal changes in mass balanc...
Published in: | The Cryosphere |
---|---|
Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2020
|
Subjects: | |
Online Access: | https://doi.org/10.5194/tc-14-3425-2020 https://tc.copernicus.org/articles/14/3425/2020/tc-14-3425-2020.pdf https://doaj.org/article/ae820bd5b66046d78ab3580afc82211c |
id |
fttriple:oai:gotriple.eu:oai:doaj.org/article:ae820bd5b66046d78ab3580afc82211c |
---|---|
record_format |
openpolar |
spelling |
fttriple:oai:gotriple.eu:oai:doaj.org/article:ae820bd5b66046d78ab3580afc82211c 2023-05-15T18:32:17+02:00 Variability in glacier albedo and links to annual mass balance for the gardens of Eden and Allah, Southern Alps, New Zealand A. J. Dowson P. Sirguey N. J. Cullen 2020-10-01 https://doi.org/10.5194/tc-14-3425-2020 https://tc.copernicus.org/articles/14/3425/2020/tc-14-3425-2020.pdf https://doaj.org/article/ae820bd5b66046d78ab3580afc82211c en eng Copernicus Publications doi:10.5194/tc-14-3425-2020 1994-0416 1994-0424 https://tc.copernicus.org/articles/14/3425/2020/tc-14-3425-2020.pdf https://doaj.org/article/ae820bd5b66046d78ab3580afc82211c undefined The Cryosphere, Vol 14, Pp 3425-3448 (2020) envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2020 fttriple https://doi.org/10.5194/tc-14-3425-2020 2023-01-22T18:11:00Z The gardens of Eden and Allah (GoEA) are two of New Zealand's largest ice fields. However, their remote location and protected conservation status have limited access and complicated monitoring and research efforts. To improve our understanding of the spatial and temporal changes in mass balance of these unique ice fields, observations from the Moderate Resolution Imaging Spectroradiometer (MODIS) sensors are used to monitor annual minimum glacier-wide albedo (α¯yrmin) over the period 2000–2018. The α¯yrmin for 12 individual glaciers ranges between 0.42 and 0.70 and can occur as early as mid-January and as late as the end of April. The evolution of the timing of α¯yrmin indicates a shift to later in the summer over the 19-year period on 10 of the 12 glaciers. However, there is only a weak relationship between the delay in timing and the magnitude of α¯yrmin, which implies that albedo is not necessarily lower if it is delayed. The largest negative departures in α¯yrmin (lower-than-average albedo) are consistent with high snowline altitudes (SLAs) relative to the long-term average as determined from the End of Summer Snowline (EOSS) survey, which has been the benchmark for monitoring glaciers in the Southern Alps for over 40 years. While the record of α¯yrmin for Vertebrae Col 25, an index glacier of the EOSS survey and one of the GoEA glaciers, explains less than half of the variability observed in the corresponding EOSS SLA (R2=0.43, p=0.003), the relationship is stronger when compared to other GoEA glaciers. Angel Glacier has the strongest relationship with EOSS observations at Vertebrae Col 25, accounting for 69 % of its variance (p<0.001). A key advantage in using the α¯yrmin approach is that it enables variability in the response of individual glaciers to be explored, revealing that topographic setting plays a key role in addition to the regional climate signal. The observed variability in individual glacier response at the scale of the GoEA contrasts with the high consistency of responses found by the ... Article in Journal/Newspaper The Cryosphere Unknown New Zealand The Cryosphere 14 10 3425 3448 |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
envir geo |
spellingShingle |
envir geo A. J. Dowson P. Sirguey N. J. Cullen Variability in glacier albedo and links to annual mass balance for the gardens of Eden and Allah, Southern Alps, New Zealand |
topic_facet |
envir geo |
description |
The gardens of Eden and Allah (GoEA) are two of New Zealand's largest ice fields. However, their remote location and protected conservation status have limited access and complicated monitoring and research efforts. To improve our understanding of the spatial and temporal changes in mass balance of these unique ice fields, observations from the Moderate Resolution Imaging Spectroradiometer (MODIS) sensors are used to monitor annual minimum glacier-wide albedo (α¯yrmin) over the period 2000–2018. The α¯yrmin for 12 individual glaciers ranges between 0.42 and 0.70 and can occur as early as mid-January and as late as the end of April. The evolution of the timing of α¯yrmin indicates a shift to later in the summer over the 19-year period on 10 of the 12 glaciers. However, there is only a weak relationship between the delay in timing and the magnitude of α¯yrmin, which implies that albedo is not necessarily lower if it is delayed. The largest negative departures in α¯yrmin (lower-than-average albedo) are consistent with high snowline altitudes (SLAs) relative to the long-term average as determined from the End of Summer Snowline (EOSS) survey, which has been the benchmark for monitoring glaciers in the Southern Alps for over 40 years. While the record of α¯yrmin for Vertebrae Col 25, an index glacier of the EOSS survey and one of the GoEA glaciers, explains less than half of the variability observed in the corresponding EOSS SLA (R2=0.43, p=0.003), the relationship is stronger when compared to other GoEA glaciers. Angel Glacier has the strongest relationship with EOSS observations at Vertebrae Col 25, accounting for 69 % of its variance (p<0.001). A key advantage in using the α¯yrmin approach is that it enables variability in the response of individual glaciers to be explored, revealing that topographic setting plays a key role in addition to the regional climate signal. The observed variability in individual glacier response at the scale of the GoEA contrasts with the high consistency of responses found by the ... |
format |
Article in Journal/Newspaper |
author |
A. J. Dowson P. Sirguey N. J. Cullen |
author_facet |
A. J. Dowson P. Sirguey N. J. Cullen |
author_sort |
A. J. Dowson |
title |
Variability in glacier albedo and links to annual mass balance for the gardens of Eden and Allah, Southern Alps, New Zealand |
title_short |
Variability in glacier albedo and links to annual mass balance for the gardens of Eden and Allah, Southern Alps, New Zealand |
title_full |
Variability in glacier albedo and links to annual mass balance for the gardens of Eden and Allah, Southern Alps, New Zealand |
title_fullStr |
Variability in glacier albedo and links to annual mass balance for the gardens of Eden and Allah, Southern Alps, New Zealand |
title_full_unstemmed |
Variability in glacier albedo and links to annual mass balance for the gardens of Eden and Allah, Southern Alps, New Zealand |
title_sort |
variability in glacier albedo and links to annual mass balance for the gardens of eden and allah, southern alps, new zealand |
publisher |
Copernicus Publications |
publishDate |
2020 |
url |
https://doi.org/10.5194/tc-14-3425-2020 https://tc.copernicus.org/articles/14/3425/2020/tc-14-3425-2020.pdf https://doaj.org/article/ae820bd5b66046d78ab3580afc82211c |
geographic |
New Zealand |
geographic_facet |
New Zealand |
genre |
The Cryosphere |
genre_facet |
The Cryosphere |
op_source |
The Cryosphere, Vol 14, Pp 3425-3448 (2020) |
op_relation |
doi:10.5194/tc-14-3425-2020 1994-0416 1994-0424 https://tc.copernicus.org/articles/14/3425/2020/tc-14-3425-2020.pdf https://doaj.org/article/ae820bd5b66046d78ab3580afc82211c |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/tc-14-3425-2020 |
container_title |
The Cryosphere |
container_volume |
14 |
container_issue |
10 |
container_start_page |
3425 |
op_container_end_page |
3448 |
_version_ |
1766216383326060544 |