The Connected Isotopic Water Cycle in the Community Earth System Model Version 1
Abstract
Abstract Because of the pervasive role of water in the Earth system, the relative abundances of stable isotopologues of water are valuable for understanding atmospheric, oceanic, and biospheric processes, and for interpreting paleoclimate proxy reconstructions. Isotopologues are transported by both large‐scale and turbulent flows, and the ratio of heavy to light isotopologues changes due to fractionation that can accompany condensation and evaporation processes. Correctly predicting the isotopic distributions requires resolving the relationships between large‐scale ocean and atmospheric circulation and smaller‐scale hydrological processes, which can be accomplished within a coupled climate modeling framework. Here we present the water isotope‐enabled version of the Community Earth System Model version 1 (iCESM1), which simulates global variations in water isotopic ratios in the atmosphere, land, ocean, and sea ice. In a transient Last Millennium simulation covering the 850–2005 period, iCESM1 correctly captures the late‐twentieth‐century structure of δ 18 O and δD over the global oceans, with more limited accuracy over land. The relationship between salinity and seawater δ 18 O is also well represented over the observational period, including interbasin variations. We illustrate the utility of coupled, isotope‐enabled simulations using both Last Millennium simulations and freshwater hosing experiments with iCESM1. Closing the isotopic mass balancemore »
- Authors:
-
[1];
[2];
[1];
[4];
[5];
[1];
[6];
[7];
[8];
[9]
- Climate and Global Dynamics Laboratory National Center for Atmospheric Research Boulder CO USA
- Bren School of Environmental Science &, Management University of California Santa Barbara CA USA
- Department of Geography The Ohio State University Columbus OH USA
- College of Earth, Ocean, &, Atmospheric Sciences Oregon State University Corvallis OR USA
- NASA Goddard Institute for Space Studies and Center for Climate Systems Research Columbia University New York NY USA
- Department of Geosciences University of Connecticut Storrs CT USA
- Department of Computer Science University of Colorado Boulder Boulder CO USA
- Center for Nonlinear Studies Los Alamos National Laboratory Los Alamos NM USA
- Department of Earth and Environmental Sciences University of Michigan Ann Arbor MI USA
- Publication Date:
- Research Org.:
- Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
- Sponsoring Org.:
- USDOE; USDOE Office of Science (SC). Biological and Environmental Research (BER) (SC-23)
- OSTI Identifier:
- 1567945
- Alternate Identifier(s):
- OSTI ID: 1566119; OSTI ID: 1567950
- Report Number(s):
- LA-UR-19-28472
Journal ID: ISSN 1942-2466
- Grant/Contract Number:
- 89233218CNA000001
- Resource Type:
- Published Article
- Journal Name:
- Journal of Advances in Modeling Earth Systems
- Additional Journal Information:
- Journal Name: Journal of Advances in Modeling Earth Systems Journal Volume: 11 Journal Issue: 8; Journal ID: ISSN 1942-2466
- Publisher:
- American Geophysical Union (AGU)
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; Earth Sciences
Citation Formats
Brady, E., Stevenson, S., Bailey, D., Liu, Z., Noone, D., Nusbaumer, J., Otto‐Bliesner, B. L., Tabor, C., Tomas, R., Wong, T., Zhang, J., and Zhu, J. The Connected Isotopic Water Cycle in the Community Earth System Model Version 1. United States: N. p., 2019.
Web. doi:10.1029/2019MS001663.
Brady, E., Stevenson, S., Bailey, D., Liu, Z., Noone, D., Nusbaumer, J., Otto‐Bliesner, B. L., Tabor, C., Tomas, R., Wong, T., Zhang, J., & Zhu, J. The Connected Isotopic Water Cycle in the Community Earth System Model Version 1. United States. https://doi.org/10.1029/2019MS001663
Brady, E., Stevenson, S., Bailey, D., Liu, Z., Noone, D., Nusbaumer, J., Otto‐Bliesner, B. L., Tabor, C., Tomas, R., Wong, T., Zhang, J., and Zhu, J. Wed .
"The Connected Isotopic Water Cycle in the Community Earth System Model Version 1". United States. https://doi.org/10.1029/2019MS001663.
@article{osti_1567945,
title = {The Connected Isotopic Water Cycle in the Community Earth System Model Version 1},
author = {Brady, E. and Stevenson, S. and Bailey, D. and Liu, Z. and Noone, D. and Nusbaumer, J. and Otto‐Bliesner, B. L. and Tabor, C. and Tomas, R. and Wong, T. and Zhang, J. and Zhu, J.},
abstractNote = {Abstract Because of the pervasive role of water in the Earth system, the relative abundances of stable isotopologues of water are valuable for understanding atmospheric, oceanic, and biospheric processes, and for interpreting paleoclimate proxy reconstructions. Isotopologues are transported by both large‐scale and turbulent flows, and the ratio of heavy to light isotopologues changes due to fractionation that can accompany condensation and evaporation processes. Correctly predicting the isotopic distributions requires resolving the relationships between large‐scale ocean and atmospheric circulation and smaller‐scale hydrological processes, which can be accomplished within a coupled climate modeling framework. Here we present the water isotope‐enabled version of the Community Earth System Model version 1 (iCESM1), which simulates global variations in water isotopic ratios in the atmosphere, land, ocean, and sea ice. In a transient Last Millennium simulation covering the 850–2005 period, iCESM1 correctly captures the late‐twentieth‐century structure of δ 18 O and δD over the global oceans, with more limited accuracy over land. The relationship between salinity and seawater δ 18 O is also well represented over the observational period, including interbasin variations. We illustrate the utility of coupled, isotope‐enabled simulations using both Last Millennium simulations and freshwater hosing experiments with iCESM1. Closing the isotopic mass balance between all components of the coupled model provides new confidence in the underlying depiction of the water cycle in CESM, while also highlighting areas where the underlying hydrologic balance can be improved. The iCESM1 is poised to be a vital community resource for ongoing model development with both modern and paleoclimate applications.},
doi = {10.1029/2019MS001663},
journal = {Journal of Advances in Modeling Earth Systems},
number = 8,
volume = 11,
place = {United States},
year = {Wed Aug 07 00:00:00 EDT 2019},
month = {Wed Aug 07 00:00:00 EDT 2019}
}
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Figures / Tables:
Figure 1: A schematic of iCESM1 showing the five major model components (iCAM, iCLM, iRTM, iPOP, and iCICE) and all of the major intercomponent fluxes that impact water isotopes. It should be noted that although some of these fluxes are only shown once, they occur for multiple components (e.g., dew/frostmore »
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