Re-evaluation of the effects of precipitation amount and temperature on precipitation δ18O at the monthly and interannual timescales

Proxy records of the oxygen isotope ratio of 18O/16O of past precipitation (δ18Op) have played an important role in revealing past hydroclimatic changes, on the basis of global observed relationships between monthly precipitation δ18Op and both precipitation amount and temperature only of a few year...

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Main Authors: Yunxia Li, Kaiyue Guang, Lijun Tian, Yiping Tian, Jiayan Li, Chenxi Yang, Zhiguo Rao
Format: Article
Language:English
Published: IWA Publishing 2023-06-01
Series:Journal of Water and Climate Change
Subjects:
Online Access:http://jwcc.iwaponline.com/content/14/6/1816
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author Yunxia Li
Kaiyue Guang
Lijun Tian
Yiping Tian
Jiayan Li
Chenxi Yang
Zhiguo Rao
author_facet Yunxia Li
Kaiyue Guang
Lijun Tian
Yiping Tian
Jiayan Li
Chenxi Yang
Zhiguo Rao
author_sort Yunxia Li
collection DOAJ
description Proxy records of the oxygen isotope ratio of 18O/16O of past precipitation (δ18Op) have played an important role in revealing past hydroclimatic changes, on the basis of global observed relationships between monthly precipitation δ18Op and both precipitation amount and temperature only of a few years as reported by Dansgaard in 1964. It is therefore crucial to systematically re-evaluate the relationships using modern instrumental data. We analysed monthly and annual mean correlations from 108 global stations over the past about 60 years. Consistent with previously reported results, monthly δ18Op values in the high latitudes (≥60°) show a significant positive correlation with temperature (referred to as ‘temperature effect’) and a negative trend with precipitation amount in the low latitudes (≤20°) (‘amount effect’). However, these correlations do not hold true for yearly mean data for more than three-quarters of the stations evaluated. This indicates that the relationships between the different temporal resolutions could be more complicated than previously thought. For the related natural archives, such as ice cores, sediments, and carbonates, further careful evaluation is required to establish the robustness of their paleoclimatic implications. HIGHLIGHTS 108 GNIP stations were collected to re-analyse the relationships between δ18Op and climate variables on monthly and interannual timescales.; The relationships between δ18Op and climate variables varied on monthly and interannual timescales.; The results implied that the change of precipitation isotopic values may not be dominated by local climate change, but more likely a response to global atmospheric circulation.;
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spelling doaj.art-86005a921a3944bbb6f7f6ae8d3325f12024-04-17T08:29:56ZengIWA PublishingJournal of Water and Climate Change2040-22442408-93542023-06-011461816183010.2166/wcc.2023.446446Re-evaluation of the effects of precipitation amount and temperature on precipitation δ18O at the monthly and interannual timescalesYunxia Li0Kaiyue Guang1Lijun Tian2Yiping Tian3Jiayan Li4Chenxi Yang5Zhiguo Rao6 Key Laboratory of Ecological and Environmental Change in Subtropical Zone, School of Geographic Sciences, Hunan Normal University, Changsha 410081, China Key Laboratory of Ecological and Environmental Change in Subtropical Zone, School of Geographic Sciences, Hunan Normal University, Changsha 410081, China Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China Key Laboratory of Ecological and Environmental Change in Subtropical Zone, School of Geographic Sciences, Hunan Normal University, Changsha 410081, China Key Laboratory of Ecological and Environmental Change in Subtropical Zone, School of Geographic Sciences, Hunan Normal University, Changsha 410081, China Key Laboratory of Ecological and Environmental Change in Subtropical Zone, School of Geographic Sciences, Hunan Normal University, Changsha 410081, China Key Laboratory of Ecological and Environmental Change in Subtropical Zone, School of Geographic Sciences, Hunan Normal University, Changsha 410081, China Proxy records of the oxygen isotope ratio of 18O/16O of past precipitation (δ18Op) have played an important role in revealing past hydroclimatic changes, on the basis of global observed relationships between monthly precipitation δ18Op and both precipitation amount and temperature only of a few years as reported by Dansgaard in 1964. It is therefore crucial to systematically re-evaluate the relationships using modern instrumental data. We analysed monthly and annual mean correlations from 108 global stations over the past about 60 years. Consistent with previously reported results, monthly δ18Op values in the high latitudes (≥60°) show a significant positive correlation with temperature (referred to as ‘temperature effect’) and a negative trend with precipitation amount in the low latitudes (≤20°) (‘amount effect’). However, these correlations do not hold true for yearly mean data for more than three-quarters of the stations evaluated. This indicates that the relationships between the different temporal resolutions could be more complicated than previously thought. For the related natural archives, such as ice cores, sediments, and carbonates, further careful evaluation is required to establish the robustness of their paleoclimatic implications. HIGHLIGHTS 108 GNIP stations were collected to re-analyse the relationships between δ18Op and climate variables on monthly and interannual timescales.; The relationships between δ18Op and climate variables varied on monthly and interannual timescales.; The results implied that the change of precipitation isotopic values may not be dominated by local climate change, but more likely a response to global atmospheric circulation.;http://jwcc.iwaponline.com/content/14/6/1816gnip stationspaleo-δ18op recordsprecipitation amount effectprecipitation δ18otemperature effect
spellingShingle Yunxia Li
Kaiyue Guang
Lijun Tian
Yiping Tian
Jiayan Li
Chenxi Yang
Zhiguo Rao
Re-evaluation of the effects of precipitation amount and temperature on precipitation δ18O at the monthly and interannual timescales
Journal of Water and Climate Change
gnip stations
paleo-δ18op records
precipitation amount effect
precipitation δ18o
temperature effect
title Re-evaluation of the effects of precipitation amount and temperature on precipitation δ18O at the monthly and interannual timescales
title_full Re-evaluation of the effects of precipitation amount and temperature on precipitation δ18O at the monthly and interannual timescales
title_fullStr Re-evaluation of the effects of precipitation amount and temperature on precipitation δ18O at the monthly and interannual timescales
title_full_unstemmed Re-evaluation of the effects of precipitation amount and temperature on precipitation δ18O at the monthly and interannual timescales
title_short Re-evaluation of the effects of precipitation amount and temperature on precipitation δ18O at the monthly and interannual timescales
title_sort re evaluation of the effects of precipitation amount and temperature on precipitation δ18o at the monthly and interannual timescales
topic gnip stations
paleo-δ18op records
precipitation amount effect
precipitation δ18o
temperature effect
url http://jwcc.iwaponline.com/content/14/6/1816
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