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The impact of different atmospheric CO2 concentrations on large scale Miocene temperature signatures

Citation

Hossain, A and Knorr, G and Jokat, W and Lohmann, G and Hochmuth, K and Gierz, P and Gohl, K and Stepanek, C, The impact of different atmospheric CO2 concentrations on large scale Miocene temperature signatures, Paleoceanography and Paleoclimatology Article e2022PA004438. ISSN 2572-4517 (2023) [Refereed Article]


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DOI: doi:10.1029/2022PA004438

Abstract

Based on inferences from proxy records the Miocene (23.035.33 Ma) was a time of amplified polar warmth compared to today. However, it remains a challenge to simulate a warm Miocene climate and pronounced polar warmth at reconstructed Miocene CO2 concentrations. Using a state-of-the-art Earth-System-Model, we implement a high-resolution paleobathymetry and simulate Miocene climate at different atmospheric CO2 concentrations. We estimate global mean surface warming of +3.1 C relative to the preindustrial at a CO2 level of 450 ppm. An increase of atmospheric CO2 from 280450 ppm provides an individual warming of ∼1.4 C, which is as strong as all other Miocene forcing contributions combined. Substantial changes in surface albedo are vital to explain Miocene surface warming. Simulated surface temperatures fit well with proxy reconstructions at low- to mid-latitudes. The high latitude cooling bias becomes less pronounced for higher CO2. At higher CO2 levels simulated Miocene climate shows a reduced polar amplification, linked to a breakdown of seasonality in the Arctic Ocean. A pronounced warming in boreal fall is detected for a CO2 increase from 280450 ppm, in comparison to weaker warming for CO2 changes from 450720 ppm. Moreover, a pronounced warming in winter is detected for a CO2 increase from 450720 ppm, in contrast to a moderate summer temperature increase, which is accompanied by a strong sea-ice concentration decline and enhanced moisture availability promotes cloud formation in summer. As a consequence planetary albedo increases and dampens the temperature response to CO2 forcing at a warmer Miocene background climate.

Item Details

Item Type:Refereed Article
Keywords:Earth System Modelling, paleobathymetry, Miocene, atmospheric CO2
Research Division:Earth Sciences
Research Group:Geoinformatics
Research Field:Computational modelling and simulation in earth sciences
Objective Division:Environmental Policy, Climate Change and Natural Hazards
Objective Group:Understanding climate change
Objective Field:Climate change models
UTAS Author:Hochmuth, K (Dr Katharina Hochmuth)
ID Code:155037
Year Published:2023
Deposited By:Oceans and Cryosphere
Deposited On:2023-01-24
Last Modified:2023-01-25
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