Calculating uncertainty for the RICE ice core continuous flow analysis water isotope record
We describe a systematic approach to the calibration and uncertainty estimation of a high-resolution continuous flow analysis (CFA) water isotope ( δ 2 H, δ 18 O) record from the Roosevelt Island Climate Evolution (RICE) Antarctic ice core. Our method establishes robust uncertainty estimates for CFA...
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ftdoajarticles:oai:doaj.org/article:6ef681869c49417297c561cd3edca137 2023-05-15T13:33:31+02:00 Calculating uncertainty for the RICE ice core continuous flow analysis water isotope record E. D. Keller W. T. Baisden N. A. N. Bertler B. D. Emanuelsson S. Canessa A. Phillips 2018-08-01T00:00:00Z https://doi.org/10.5194/amt-11-4725-2018 https://doaj.org/article/6ef681869c49417297c561cd3edca137 EN eng Copernicus Publications https://www.atmos-meas-tech.net/11/4725/2018/amt-11-4725-2018.pdf https://doaj.org/toc/1867-1381 https://doaj.org/toc/1867-8548 doi:10.5194/amt-11-4725-2018 1867-1381 1867-8548 https://doaj.org/article/6ef681869c49417297c561cd3edca137 Atmospheric Measurement Techniques, Vol 11, Pp 4725-4736 (2018) Environmental engineering TA170-171 Earthwork. Foundations TA715-787 article 2018 ftdoajarticles https://doi.org/10.5194/amt-11-4725-2018 2022-12-30T21:26:35Z We describe a systematic approach to the calibration and uncertainty estimation of a high-resolution continuous flow analysis (CFA) water isotope ( δ 2 H, δ 18 O) record from the Roosevelt Island Climate Evolution (RICE) Antarctic ice core. Our method establishes robust uncertainty estimates for CFA δ 2 H and δ 18 O measurements, comparable to those reported for discrete sample δ 2 H and δ 18 O analysis. Data were calibrated using a time-weighted two-point linear calibration with two standards measured both before and after continuously melting 3 or 4 m of ice core. The error at each data point was calculated as the quadrature sum of three factors: Allan variance error, scatter over our averaging interval (error of the variance) and calibration error (error of the mean). Final mean total uncertainty for the entire record is δ 2 H = 0.74 ‰ and δ 18 O = 0.21 ‰. Uncertainties vary through the data set and were exacerbated by a range of factors, which typically could not be isolated due to the requirements of the multi-instrument CFA campaign. These factors likely occurred in combination and included ice quality, ice breaks, upstream equipment failure, contamination with drill fluid and leaks or valve degradation. We demonstrate that our methodology for documenting uncertainty was effective across periods of uneven system performance and delivered a significant achievement in the precision of high-resolution CFA water isotope measurements. Article in Journal/Newspaper Antarc* Antarctic ice core Roosevelt Island Directory of Open Access Journals: DOAJ Articles Antarctic Roosevelt Island ENVELOPE(-162.000,-162.000,-79.283,-79.283) Atmospheric Measurement Techniques 11 8 4725 4736 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental engineering TA170-171 Earthwork. Foundations TA715-787 |
spellingShingle |
Environmental engineering TA170-171 Earthwork. Foundations TA715-787 E. D. Keller W. T. Baisden N. A. N. Bertler B. D. Emanuelsson S. Canessa A. Phillips Calculating uncertainty for the RICE ice core continuous flow analysis water isotope record |
topic_facet |
Environmental engineering TA170-171 Earthwork. Foundations TA715-787 |
description |
We describe a systematic approach to the calibration and uncertainty estimation of a high-resolution continuous flow analysis (CFA) water isotope ( δ 2 H, δ 18 O) record from the Roosevelt Island Climate Evolution (RICE) Antarctic ice core. Our method establishes robust uncertainty estimates for CFA δ 2 H and δ 18 O measurements, comparable to those reported for discrete sample δ 2 H and δ 18 O analysis. Data were calibrated using a time-weighted two-point linear calibration with two standards measured both before and after continuously melting 3 or 4 m of ice core. The error at each data point was calculated as the quadrature sum of three factors: Allan variance error, scatter over our averaging interval (error of the variance) and calibration error (error of the mean). Final mean total uncertainty for the entire record is δ 2 H = 0.74 ‰ and δ 18 O = 0.21 ‰. Uncertainties vary through the data set and were exacerbated by a range of factors, which typically could not be isolated due to the requirements of the multi-instrument CFA campaign. These factors likely occurred in combination and included ice quality, ice breaks, upstream equipment failure, contamination with drill fluid and leaks or valve degradation. We demonstrate that our methodology for documenting uncertainty was effective across periods of uneven system performance and delivered a significant achievement in the precision of high-resolution CFA water isotope measurements. |
format |
Article in Journal/Newspaper |
author |
E. D. Keller W. T. Baisden N. A. N. Bertler B. D. Emanuelsson S. Canessa A. Phillips |
author_facet |
E. D. Keller W. T. Baisden N. A. N. Bertler B. D. Emanuelsson S. Canessa A. Phillips |
author_sort |
E. D. Keller |
title |
Calculating uncertainty for the RICE ice core continuous flow analysis water isotope record |
title_short |
Calculating uncertainty for the RICE ice core continuous flow analysis water isotope record |
title_full |
Calculating uncertainty for the RICE ice core continuous flow analysis water isotope record |
title_fullStr |
Calculating uncertainty for the RICE ice core continuous flow analysis water isotope record |
title_full_unstemmed |
Calculating uncertainty for the RICE ice core continuous flow analysis water isotope record |
title_sort |
calculating uncertainty for the rice ice core continuous flow analysis water isotope record |
publisher |
Copernicus Publications |
publishDate |
2018 |
url |
https://doi.org/10.5194/amt-11-4725-2018 https://doaj.org/article/6ef681869c49417297c561cd3edca137 |
long_lat |
ENVELOPE(-162.000,-162.000,-79.283,-79.283) |
geographic |
Antarctic Roosevelt Island |
geographic_facet |
Antarctic Roosevelt Island |
genre |
Antarc* Antarctic ice core Roosevelt Island |
genre_facet |
Antarc* Antarctic ice core Roosevelt Island |
op_source |
Atmospheric Measurement Techniques, Vol 11, Pp 4725-4736 (2018) |
op_relation |
https://www.atmos-meas-tech.net/11/4725/2018/amt-11-4725-2018.pdf https://doaj.org/toc/1867-1381 https://doaj.org/toc/1867-8548 doi:10.5194/amt-11-4725-2018 1867-1381 1867-8548 https://doaj.org/article/6ef681869c49417297c561cd3edca137 |
op_doi |
https://doi.org/10.5194/amt-11-4725-2018 |
container_title |
Atmospheric Measurement Techniques |
container_volume |
11 |
container_issue |
8 |
container_start_page |
4725 |
op_container_end_page |
4736 |
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1766043128570052608 |