Preprints
https://doi.org/10.5194/cp-2024-30
https://doi.org/10.5194/cp-2024-30
24 May 2024
 | 24 May 2024
Status: this preprint is currently under review for the journal CP.

Response of Late-Eocene warmth to incipient glaciation on Antarctica

Dennis H.A. Vermeulen, Michiel L. J. Baatsen, and Anna S. von der Heydt

Abstract. The Eocene-Oligocene Transition (EOT) is marked by a sudden δ18O excursion occurring in two distinct phases, ~500 ky apart. These phases signal a shift from the warm Middle- to Late-Eocene greenhouse climate to cooler conditions, with global surface air temperatures decreasing by 3–5 °C and the emergence of the first continent-wide Antarctic Ice Sheet (AIS). While ice-sheet modelling suggests that ice sheet growth can be triggered by declining pCO2, it still remains unclear how this transition has been initiated, in particular the first growth phase that seems to be related to oceanic and atmospheric cooling rather than ice sheet growth. Recent climate model simulations of the Late-Eocene show improved accuracy but depict climatic conditions that are not conducive to the survival of incipient ice sheets throughout the summer season. This study therefore examines whether it is plausible to develop ice sheets of sufficient scale to trigger the feedback mechanism(s) required to disrupt the atmospheric regime above the Antarctic continent during warm Late-Eocene summers and establish more favourable conditions for ice expansion. We thereby aim to assess the stability of an incipient AIS under varying radiative, orbital and cryospheric forcing. To do so, we evaluate Community Earth System Model 1.0.5 simulations, using a 38 Ma geo- and topographical reconstruction, considering different radiative (4 and 2 pre-industrial carbon) and orbital (present-day and low summer insolation) forcings. The climatic conditions prevailing during (the lead-up to) the EOT can be characterised as extremely seasonal and monsoonal, featuring a short yet intense summer period and contrasting cold winters — highly inhospitable to ice sheet growth for most of the continent, as limited snow accumulation is expected to survive the summer season. A narrow convergence zone with moist convection around the region where sub-cloud equivalent potential temperature is high is shown to exhibit a ring-like structure, advecting moist surface air advected from the Southern Ocean. This advection leads to high values of moist static energy and subsequent precipitation in these regions. To assess the influence of cryospheric forcing, we conducted another simulation, with regional, moderately-sized ice sheets imposed on the continent, to investigate their stability and influence on the atmospheric circulation. Regionally, these relatively small ice sheets respond strongly to radiative and orbital forcing, and demonstrate remarkably favourable self-sustaining and even expansion potential under 2 PIC and low summer insolation conditions. This emphasises a significant hysteresis effect for local and/or regional ice sheets on the Antarctic continent, suggesting the potential for a significant volume of ice on the Antarctic continent without an imminent full glaciation prior to the EOT.

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Dennis H.A. Vermeulen, Michiel L. J. Baatsen, and Anna S. von der Heydt

Status: open (until 19 Jul 2024)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
Dennis H.A. Vermeulen, Michiel L. J. Baatsen, and Anna S. von der Heydt

Data sets

4PIC, 2PIC/s, 2PIC/l and 2PIC/li data set Dennis Vermeulen, Michiel Baatsen, and Anna von der Heydt https://doi.org/10.24416/UU01-A0VMKZ

Model code and software

4PIC, 2PIC/s, 2PIC/l and 2PIC/li analysis code Dennis Vermeulen, Michiel Baatsen, and Anna von der Heydt https://doi.org/10.24416/UU01-A0VMKZ

Dennis H.A. Vermeulen, Michiel L. J. Baatsen, and Anna S. von der Heydt

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Short summary
Late-Eocene summers, 34 million years ago, were hot on Antarctica, with temperatures up to 30 °C. We also know that during that period the first Antarctic Ice Sheet formed. Since climate models don’t show this transition from warm climate to ice sheet formation accurately, we imposed regional ice sheets onto the continent in a realistic climate, and show that these ice sheets don't melt away. This suggests that the initiation of ice sheet growth might indeed have happened during warmer periods.