Water isotopes, climate variability, and the hydrological cycle: recent advances and new frontiers
The hydrologic cycle is a fundamental component of the climate system with critical societal and ecological relevance. Yet gaps persist in our understanding of water fluxes and their response to increased greenhouse gas forcing. The stable isotope ratios of oxygen and hydrogen in water provide a uni...
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Published in | Environmental Research: Climate Vol. 2; no. 2; pp. 22002 - 22028 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
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IOP Publishing
01.06.2023
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Abstract | The hydrologic cycle is a fundamental component of the climate system with critical societal and ecological relevance. Yet gaps persist in our understanding of water fluxes and their response to increased greenhouse gas forcing. The stable isotope ratios of oxygen and hydrogen in water provide a unique opportunity to evaluate hydrological processes and investigate their role in the variability of the climate system and its sensitivity to change. Water isotopes also form the basis of many paleoclimate proxies in a variety of archives, including ice cores, lake and marine sediments, corals, and speleothems. These records hold most of the available information about past hydrologic variability prior to instrumental observations. Water isotopes thus provide a ‘common currency’ that links paleoclimate archives to modern observations, allowing us to evaluate hydrologic processes and their effects on climate variability on a wide range of time and length scales. Building on previous literature summarizing advancements in water isotopic measurements and modeling and describe water isotopic applications for understanding hydrological processes, this topical review reflects on new insights about climate variability from isotopic studies. We highlight new work and opportunities to enhance our understanding and predictive skill and offer a set of recommendations to advance observational and model-based tools for climate research. Finally, we highlight opportunities to better constrain climate sensitivity and identify anthropogenically-driven hydrologic changes within the inherently noisy background of natural climate variability. |
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AbstractList | The hydrologic cycle is a fundamental component of the climate system with critical societal and ecological relevance. Yet gaps persist in our understanding of water fluxes and their response to increased greenhouse gas forcing. The stable isotope ratios of oxygen and hydrogen in water provide a unique opportunity to evaluate hydrological processes and investigate their role in the variability of the climate system and its sensitivity to change. Water isotopes also form the basis of many paleoclimate proxies in a variety of archives, including ice cores, lake and marine sediments, corals, and speleothems. These records hold most of the available information about past hydrologic variability prior to instrumental observations. Water isotopes thus provide a ‘common currency’ that links paleoclimate archives to modern observations, allowing us to evaluate hydrologic processes and their effects on climate variability on a wide range of time and length scales. Building on previous literature summarizing advancements in water isotopic measurements and modeling and describe water isotopic applications for understanding hydrological processes, this topical review reflects on new insights about climate variability from isotopic studies. We highlight new work and opportunities to enhance our understanding and predictive skill and offer a set of recommendations to advance observational and model-based tools for climate research. Finally, we highlight opportunities to better constrain climate sensitivity and identify anthropogenically-driven hydrologic changes within the inherently noisy background of natural climate variability. Abstract The hydrologic cycle is a fundamental component of the climate system with critical societal and ecological relevance. Yet gaps persist in our understanding of water fluxes and their response to increased greenhouse gas forcing. The stable isotope ratios of oxygen and hydrogen in water provide a unique opportunity to evaluate hydrological processes and investigate their role in the variability of the climate system and its sensitivity to change. Water isotopes also form the basis of many paleoclimate proxies in a variety of archives, including ice cores, lake and marine sediments, corals, and speleothems. These records hold most of the available information about past hydrologic variability prior to instrumental observations. Water isotopes thus provide a ‘common currency’ that links paleoclimate archives to modern observations, allowing us to evaluate hydrologic processes and their effects on climate variability on a wide range of time and length scales. Building on previous literature summarizing advancements in water isotopic measurements and modeling and describe water isotopic applications for understanding hydrological processes, this topical review reflects on new insights about climate variability from isotopic studies. Our intention is to highlight new work and opportunities to enhance our understanding and predictive skill, rather than be exhaustive. We offer a set of recommendations to advance observational and model-based tools for climate research, and highlight opportunities to better constrain climate sensitivity and identify anthropogenically-driven hydrologic changes within the inherently noisy background of natural climate variability. |
Author | Dee, Sylvia Noone, David Bailey, Adriana Nusbaumer, Jesse Atwood, Alyssa Conroy, Jessica L Stevenson, Samantha |
Author_xml | – sequence: 1 givenname: Sylvia orcidid: 0000-0002-2140-785X surname: Dee fullname: Dee, Sylvia organization: Environmental, and Planetary Sciences Rice University, Department of Earth, Houston, TX 77005, United States of America – sequence: 2 givenname: Adriana orcidid: 0000-0002-2614-1560 surname: Bailey fullname: Bailey, Adriana organization: National Center for Atmospheric Research , Boulder, CO 80301, United States of America – sequence: 3 givenname: Jessica L orcidid: 0000-0003-3652-3199 surname: Conroy fullname: Conroy, Jessica L organization: University of Illinois at Urbana-Champaign Department of Earth Science & Environmental Change, Urbana, IL 61801, United States of America – sequence: 4 givenname: Alyssa orcidid: 0000-0001-6615-6540 surname: Atwood fullname: Atwood, Alyssa organization: Florida State University Department of Earth, Ocean and Atmospheric Science, Tallahassee, FL 32306, United States of America – sequence: 5 givenname: Samantha orcidid: 0000-0002-1223-8521 surname: Stevenson fullname: Stevenson, Samantha organization: University of California, Santa Barbara, Bren School of Environmental Science and Management , Santa Barbara, CA 93106, United States of America – sequence: 6 givenname: Jesse orcidid: 0000-0002-4370-3537 surname: Nusbaumer fullname: Nusbaumer, Jesse organization: National Center for Atmospheric Research , Boulder, CO 80301, United States of America – sequence: 7 givenname: David orcidid: 0000-0002-8642-7843 surname: Noone fullname: Noone, David organization: University of Auckland Department of Physics, Auckland, New Zealand |
BackLink | https://www.osti.gov/biblio/1969420$$D View this record in Osti.gov |
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Snippet | The hydrologic cycle is a fundamental component of the climate system with critical societal and ecological relevance. Yet gaps persist in our understanding of... Abstract The hydrologic cycle is a fundamental component of the climate system with critical societal and ecological relevance. Yet gaps persist in our... |
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SubjectTerms | climate change climate variablity hydrological cycle paleoclimate water isotopes |
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Title | Water isotopes, climate variability, and the hydrological cycle: recent advances and new frontiers |
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