November 1, 2020 Journal article Open Access

Robert A. Tomas; Sarah L. Shafer; Gunter R. Leguy; Esther C. Brady; Natalie M. Mahowald; Peter Lawrence; Aleah Sommers; Patrick J. Bartlein; Bette L. Otto-Bliesner; Samuel Albani; Erik Kluzek; Mathew Rothstein

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{
  "@context": "https://schema.org/", 
  "@id": "https://doi.org/10.1029/2020pa003957", 
  "@type": "ScholarlyArticle", 
  "creator": [
    {
      "@type": "Person", 
      "name": "Robert A. Tomas"
    }, 
    {
      "@type": "Person", 
      "name": "Sarah L. Shafer"
    }, 
    {
      "@type": "Person", 
      "name": "Gunter R. Leguy"
    }, 
    {
      "@type": "Person", 
      "name": "Esther C. Brady"
    }, 
    {
      "@type": "Person", 
      "name": "Natalie M. Mahowald"
    }, 
    {
      "@type": "Person", 
      "name": "Peter Lawrence"
    }, 
    {
      "@type": "Person", 
      "name": "Aleah Sommers"
    }, 
    {
      "@type": "Person", 
      "name": "Patrick J. Bartlein"
    }, 
    {
      "@type": "Person", 
      "name": "Bette L. Otto-Bliesner"
    }, 
    {
      "@type": "Person", 
      "name": "Samuel Albani"
    }, 
    {
      "@type": "Person", 
      "name": "Erik Kluzek"
    }, 
    {
      "@type": "Person", 
      "name": "Mathew Rothstein"
    }
  ], 
  "datePublished": "2020-11-01", 
  "description": "AbstractResults are presented and compared for the Community Earth System Model version 2 (CESM2) simulations of the middle Holocene (MH, 6\u00a0ka) and Last Interglacial (LIG, 127\u00a0ka). These simulations are designated as Tier 1 experiments (midHolocene and lig127k) for the Coupled Model Intercomparison Project phase 6 (CMIP6) and the Paleoclimate Modeling Intercomparison Project phase 4 (PMIP4). They use the low\u2010top, standard 1\u00b0 version of CESM2 contributing to CMIP6 DECK, historical, and future projection simulations, and to other modeling intercomparison projects. The midHolocene and lig127k provide the opportunity to examine the responses in CESM2 to the orbitally induced changes in the seasonal and latitudinal distribution of insolation. The insolation anomalies result in summer warming over the Northern Hemisphere continents, reduced Arctic summer minimum sea ice, and increased areal extent of the North African monsoon. The Arctic remains warm throughout the year. These changes are greater in the lig127k than midHolocene simulation. Other notable changes are reduction of the Ni\u00f1o3.4 variability and Drake Passage transport and a small increase in the Atlantic Meridional Overturning Circulation from the piControl to midHolocene to lig127k simulation. Comparisons to paleo\u2010data and to simulations from previous model versions are discussed. Possible reasons for mismatches with the paleo\u2010observations are proposed, including missing processes in CESM2, simplifications in the CMIP6 protocols for these experiments, and dating and calibration uncertainties in the data reconstructions.", 
  "headline": "A Comparison of the CMIP6 midHolocene and lig127k Simulations in CESM2", 
  "identifier": "https://doi.org/10.1029/2020pa003957", 
  "image": "https://zenodo.org/static/img/logos/zenodo-gradient-round.svg", 
  "inLanguage": {
    "@type": "Language", 
    "alternateName": "eng", 
    "name": "English"
  }, 
  "keywords": [
    "NSF", 
    "National Science Foundation", 
    "Division of Atmospheric and Geospace Sciences", 
    "Directorate for Geosciences", 
    "Paleontology", 
    "Atmospheric Science", 
    "Oceanography"
  ], 
  "license": "https://creativecommons.org/licenses/by/4.0/", 
  "name": "A Comparison of the CMIP6 midHolocene and lig127k Simulations in CESM2", 
  "url": "https://www.openaccessrepository.it/record/92003"
}