Hydroclimate records reveal how water cycle on Earth responds to temperature increases

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Australia; International

An international research collaboration including ANSTO has found that the global water cycle and atmospheric circulation patterns can adjust relatively quickly—within a few decades—in response to changes in the Earth's temperature and have done so in the past.

Media release

From: Australian Nuclear Science and Technology Organisation (ANSTO)

With the UN Climate Change Conference COP28 currently being held in Saudi Arabia, ANSTO is sharing a research highlight that captures our capabilities and expertise in analysing complex environmental processes.  This work is part of environmental research that encompasses water resources, the impact of contaminants and responses to climate change.

Environmental research recently published in Nature Geoscience reveals that the global water cycle and atmospheric circulation patterns can adjust relatively quickly—within a few decades—in response to changes in the Earth's temperature and has done so in the past.

This research presented preliminary proof of a close relationship between temperature and the isotopic profile of environmental waters during intermediate time scales—spanning from decades to centuries.

n this study, environmental scientists working in the Past Global Changes (PAGES) Iso2k project, including Dr Matthew Fischer at ANSTO, undertook an exhaustive analysis of the stable isotopes of hydrogen (2H) and oxygen (18O) as recorded in data sources covering the last 2000 years.

The large international team was able to determine the leading principal components and identify trends in Iso2k records.

The stable isotopes of 2H and 18O in precipitation, meteoric water (derived from precipitation, such as lakes, rivers and ice melts), and seawater can give insights into water-related processes on small and large scales. These isotopes become incorporated in natural archives like speleothems, tree rings, corals, and ice cores, which form the Iso2k database.

Standardisation of data was an essential step, and the team expanded previous work.

First author Assistant Professor Bronwen Konecky at Washington University in St. Louis explained in an article on the university website that “Every archive is different.“

“To make matters more complicated, datasets from different archives are generated by different scientific communities with their own terminology, norms and reference materials.

“We came up with data description fields (metadata) for the database that translates each record’s particularities into a common tongue that makes it possible to compare variations in one archive to variations in another.”

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ANSTO is a leader in the use of stable isotopes in environmental research. Dr Fischer used his expertise in statistical analysis and theoretical modelling to contribute to the complex, gargantuan project.

It involved collecting and collating 759 globally distributed palaeoclimate records and an analysis of hydroclimatic variables.

The time-series datasets in the Past Global Changes (PAGES) Iso2k database represent the world’s largest integrated database of water isotope proxy records.

Multimedia

Dataset spanning 30 years (850 to 1840) from the Iso2k15 records
Dataset spanning 30 years (850 to 1840) from the Iso2k15 records

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Media Release Australian Nuclear Science and Technology Organisation (ANSTO), Web page
Research Springer Nature, Web page
Journal/
conference:
Nature Geoscience
Research:Paper
Organisation/s: Australian Nuclear Science and Technology Organisation (ANSTO), Support for this work includes NSF-AGS 1805141, NSF-AGS PRF 1433408 and a David and Lucile Packard Foundation Fellowship in Science and Engineering to B.L.K.; NSF-1948746 to N.P.M.; Australian Research Council through a Discovery Project (DP170100557) and the Centre of Excellence for Climate Extremes (CE170100023) to G.M.F.; NSF-AGS 1805143 and NSF-OCE-2202794 to S.L.S.; NSF-CAREER 2145725, NSF 2103035 and NSF 2002444 to A.R.A.; NSF-CAREER 1945479, NSF 1931242 and NSF 2002460 to D.M.T.; Australian Research Council Discovery Project DP190102782 to J.J.T.; South Central Climate Adaptation Science Center Cooperative Agreement G19AC00086, NSF-2102931 and NSF- 1805702 to K.L.D.; RYC‐2013‐14073 programme and LINKA20102 and CEX2018‐000794‐S projects to B.M.; NSF-EAR PRF 1349595, NSF-EAR-IF 1652274, NSF-OPP 1504267, NSF-OPP 1737716 and NSF-CAREER 2044616 to E.K.T.; NSF-CAREER 1847791 to J.L.C.; National Oceanic and Atmospheric Administration award number NA18OAR4310427 to S.G.D.; PalMod, the German palaeoclimate modelling initiative, part of the Research for Sustainable Development initiative funded by the German Federal Ministry of Education and Research (BMBF; 01LP1922A) to L.J.; RSF project 21-17- 00006 to O.V.C.(S.); German Research Foundation grants OP217/2- 1, OP217/3-1, OP217/4-1 to T.O.; Natural Sciences and Engineering Research Council of Canada Discovery Grant RGPIN-2016-06730 to T.J.P.; Australian Research Council Project (LP210300691) to G.S.; Australian Research Council through a Future Fellowship (FT160100029), Special Research Initiative for the Australian Centre for Excellence in Antarctic Science (SR200100008) and the Centre of Excellence for Climate Extremes (CE170100023) to N.J.A; Natural Sciences and Engineering Research Council of Canada Discovery Grant RGPIN-2021-03888 to A.J.O.; and Australian Antarctic Science (AAS) grants 757, 4061, 4062 and 4537 to M.C. and A.M.
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