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The Connected Isotopic Water Cycle in the Community Earth System Model Version 1
dc.contributor.authorBrady, E.
dc.contributor.authorStevenson, S.
dc.contributor.authorBailey, D.
dc.contributor.authorLiu, Z.
dc.contributor.authorNoone, D.
dc.contributor.authorNusbaumer, J.
dc.contributor.authorOtto‐bliesner, B. L.
dc.contributor.authorTabor, C.
dc.contributor.authorTomas, R.
dc.contributor.authorWong, T.
dc.contributor.authorZhang, J.
dc.contributor.authorZhu, J.
dc.date.accessioned2019-10-30T15:30:27Z
dc.date.availableWITHHELD_11_MONTHS
dc.date.available2019-10-30T15:30:27Z
dc.date.issued2019-08
dc.identifier.citationBrady, 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. (2019). "The Connected Isotopic Water Cycle in the Community Earth System Model Version 1." Journal of Advances in Modeling Earth Systems 11(8): 2547-2566.
dc.identifier.issn1942-2466
dc.identifier.issn1942-2466
dc.identifier.urihttps://hdl.handle.net/2027.42/151857
dc.description.abstractBecause 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 largeâ 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 largeâ scale ocean and atmospheric circulation and smallerâ scale hydrological processes, which can be accomplished within a coupled climate modeling framework. Here we present the water isotopeâ 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 850â 2005 period, iCESM1 correctly captures the lateâ twentiethâ century structure of δ18O and δD over the global oceans, with more limited accuracy over land. The relationship between salinity and seawater δ18O is also well represented over the observational period, including interbasin variations. We illustrate the utility of coupled, isotopeâ 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.Key PointsAn isotopeâ enabled version of the Community Earth System Model (iCESM1) is now publicly availableiCESM1 simulates the major observed features of δ18O and δD over the late twentieth centuryiCESM1 is useful for both modern climate and paleoclimate applications
dc.publisherNOAA
dc.publisherWiley Periodicals, Inc.
dc.subject.otherwater isotopologues
dc.subject.otherclimate modeling
dc.subject.otherCESM
dc.titleThe Connected Isotopic Water Cycle in the Community Earth System Model Version 1
dc.typeArticle
dc.rights.robotsIndexNoFollow
dc.subject.hlbsecondlevelGeological Sciences
dc.subject.hlbtoplevelScience
dc.description.peerreviewedPeer Reviewed
dc.description.bitstreamurlhttps://deepblue.lib.umich.edu/bitstream/2027.42/151857/1/jame20931.pdf
dc.description.bitstreamurlhttps://deepblue.lib.umich.edu/bitstream/2027.42/151857/2/jame20931_am.pdf
dc.identifier.doi10.1029/2019MS001663
dc.identifier.sourceJournal of Advances in Modeling Earth Systems
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