The response of glaciers to climatic persistence
The attribution of past glacier length fluctuations to changes in climate requires characterizing glacier mass-balance variability. Observational records, which are relatively short, are consistent with random fluctuations uncorrelated in time, plus an anthropogenic trend. However, longer records of...
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Cambridge University Press
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Online Access: | https://doi.org/10.1017/jog.2016.4 https://doaj.org/article/b66f6d263c914ebdbf18a25a3ae3e545 |
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ftdoajarticles:oai:doaj.org/article:b66f6d263c914ebdbf18a25a3ae3e545 2023-05-15T16:57:35+02:00 The response of glaciers to climatic persistence GERARD H. ROE MARCIA B. BAKER 2016-06-01T00:00:00Z https://doi.org/10.1017/jog.2016.4 https://doaj.org/article/b66f6d263c914ebdbf18a25a3ae3e545 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143016000046/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.4 0022-1430 1727-5652 https://doaj.org/article/b66f6d263c914ebdbf18a25a3ae3e545 Journal of Glaciology, Vol 62, Pp 440-450 (2016) climate persistence glacier fluctuations natural variability Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2016 ftdoajarticles https://doi.org/10.1017/jog.2016.4 2023-03-12T01:30:59Z The attribution of past glacier length fluctuations to changes in climate requires characterizing glacier mass-balance variability. Observational records, which are relatively short, are consistent with random fluctuations uncorrelated in time, plus an anthropogenic trend. However, longer records of other climate variables suggest that, in fact, there is a degree of temporal persistence associated with internal (i.e. unforced) climate variability, and that it varies with location and climate. Therefore, it is likely that persistence does exist for mass balance, but records are too short to confirm its presence, or establish its magnitude, with conventional statistical tests. Extending the previous work, we explore the impact of potential climatic persistence on glacier length fluctuations. We use a numerical model and a newly developed analytical model to establish that persistence, even of a degree so small as to be effectively undetectable in the longest mass-balance records, can significantly enhance the resulting glacier length fluctuations. This has a big impact on glacier-excursion probabilities: what was an extremely unlikely event (<1%) can become virtually certain (>99%), when persistence is incorporated. Since the actual degree of climatic persistence that applies to any given glacier is hard to establish, these results complicate the attribution of past glacier changes. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 62 233 440 450 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
climate persistence glacier fluctuations natural variability Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
climate persistence glacier fluctuations natural variability Environmental sciences GE1-350 Meteorology. Climatology QC851-999 GERARD H. ROE MARCIA B. BAKER The response of glaciers to climatic persistence |
topic_facet |
climate persistence glacier fluctuations natural variability Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
The attribution of past glacier length fluctuations to changes in climate requires characterizing glacier mass-balance variability. Observational records, which are relatively short, are consistent with random fluctuations uncorrelated in time, plus an anthropogenic trend. However, longer records of other climate variables suggest that, in fact, there is a degree of temporal persistence associated with internal (i.e. unforced) climate variability, and that it varies with location and climate. Therefore, it is likely that persistence does exist for mass balance, but records are too short to confirm its presence, or establish its magnitude, with conventional statistical tests. Extending the previous work, we explore the impact of potential climatic persistence on glacier length fluctuations. We use a numerical model and a newly developed analytical model to establish that persistence, even of a degree so small as to be effectively undetectable in the longest mass-balance records, can significantly enhance the resulting glacier length fluctuations. This has a big impact on glacier-excursion probabilities: what was an extremely unlikely event (<1%) can become virtually certain (>99%), when persistence is incorporated. Since the actual degree of climatic persistence that applies to any given glacier is hard to establish, these results complicate the attribution of past glacier changes. |
format |
Article in Journal/Newspaper |
author |
GERARD H. ROE MARCIA B. BAKER |
author_facet |
GERARD H. ROE MARCIA B. BAKER |
author_sort |
GERARD H. ROE |
title |
The response of glaciers to climatic persistence |
title_short |
The response of glaciers to climatic persistence |
title_full |
The response of glaciers to climatic persistence |
title_fullStr |
The response of glaciers to climatic persistence |
title_full_unstemmed |
The response of glaciers to climatic persistence |
title_sort |
response of glaciers to climatic persistence |
publisher |
Cambridge University Press |
publishDate |
2016 |
url |
https://doi.org/10.1017/jog.2016.4 https://doaj.org/article/b66f6d263c914ebdbf18a25a3ae3e545 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 62, Pp 440-450 (2016) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143016000046/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2016.4 0022-1430 1727-5652 https://doaj.org/article/b66f6d263c914ebdbf18a25a3ae3e545 |
op_doi |
https://doi.org/10.1017/jog.2016.4 |
container_title |
Journal of Glaciology |
container_volume |
62 |
container_issue |
233 |
container_start_page |
440 |
op_container_end_page |
450 |
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1766049148320088064 |