Preprints
https://doi.org/10.5194/egusphere-2023-380
https://doi.org/10.5194/egusphere-2023-380
17 Mar 2023
 | 17 Mar 2023

Quantifying Effects of Earth Orbital Parameters and Greenhouse Gases on Mid-Holocene Climate

Yibo Kang and Haijun Yang

Abstract. The mid-Holocene (MH) is the most recent typical climate period and a hot topic for global paleocultural research. Following the latest Paleoclimate Modelling Intercomparison Project (PMIP) protocol and using a fully coupled climate model, we simulated the climate difference between the MH and the pre-industrial (PI) periods, and quantified the effects of Earth orbital parameters (ORB) and greenhouse gases (GHG) on climate difference. More attention was paid to the simulated differences in the Atlantic meridional overturning circulation (AMOC) between these two periods. Compared to the PI conditions, the ORB effect in the MH simulation led to the seasonal enhancement of temperature, consistent with previous findings. For the MH simulation, the ORB effect led to a remarkably warmer climate in the mid-high latitudes and increased precipitation in the Northern Hemisphere, which were partially offset by the cooling effect of the lower GHG. The AMOC in the MH simulation was about 4 % stronger than that in the PI conditions. The ORB effect led to 6 % enhancement of the AMOC in the MH simulation, which was, however, partly neutralized by the GHG effect. The simulated stronger AMOC in the MH was mainly due to the thinner sea ice in the polar oceans caused by the ORB effect, which reduced the freshwater flux export to the subpolar Atlantic and resulted in a more saline North Atlantic. This study may help us quantitatively understand the role of different external forcing factors in the Earth’s climate evolution since the MH.

Yibo Kang and Haijun Yang

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-380', Anonymous Referee #1, 02 May 2023
    • AC1: 'Reply on RC1', Haijun Yang, 09 May 2023
  • RC2: 'Comment on egusphere-2023-380', Chris Brierley, 05 May 2023
    • AC2: 'Reply on RC2', Haijun Yang, 09 May 2023
      • RC3: 'Reply on AC2', Chris Brierley, 11 May 2023
        • AC3: 'Reply on RC3', Haijun Yang, 11 May 2023
          • RC4: 'Reply on AC3', Chris Brierley, 12 May 2023
            • AC4: 'Reply on RC4', Haijun Yang, 13 May 2023

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-380', Anonymous Referee #1, 02 May 2023
    • AC1: 'Reply on RC1', Haijun Yang, 09 May 2023
  • RC2: 'Comment on egusphere-2023-380', Chris Brierley, 05 May 2023
    • AC2: 'Reply on RC2', Haijun Yang, 09 May 2023
      • RC3: 'Reply on AC2', Chris Brierley, 11 May 2023
        • AC3: 'Reply on RC3', Haijun Yang, 11 May 2023
          • RC4: 'Reply on AC3', Chris Brierley, 12 May 2023
            • AC4: 'Reply on RC4', Haijun Yang, 13 May 2023

Yibo Kang and Haijun Yang

Yibo Kang and Haijun Yang

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Short summary
We simulated the climate difference between the MH and the pre-industrial (PI) periods, and quantified the effects of Earth orbital parameters (ORB) and greenhouse gases (GHG) on climate difference. We think the insignificant difference of the Atlantic Meridional Overturning Circulation between the MH and PI periods is resulted from competing effects of the ORB and the GHG on the climate.