Considerable Uncertainty of Simulated Arctic Temperature Change in the Mid‐Holocene Due To Initial Ocean Perturbation

Abstract Arctic temperature is one of the most uncertain aspects of mid‐Holocene (MH) climate change modeling, usually attributed to the different responses of different models to external forcing. However, in this study, we find that significant discrepancies (i.e., the noise is close to the signal...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Jian Shi, Gerrit Lohmann
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
mid‐Holocene
Arctic temperature
uncertainty
modeling
initial perturbation
Geophysics. Cosmic physics
QC801-809
albedo
Climate change
Sea ice
Online Access:https://doi.org/10.1029/2023GL106337
https://doaj.org/article/75bf4604a2394e969dd5f9e3c5ddd0ca
Description
Summary:Abstract Arctic temperature is one of the most uncertain aspects of mid‐Holocene (MH) climate change modeling, usually attributed to the different responses of different models to external forcing. However, in this study, we find that significant discrepancies (i.e., the noise is close to the signal in term of climate change) in the MH Arctic temperature changes can occur within the same model and for identical external forcing due to initial ocean condition perturbations. It is shown that initial ocean perturbations can affect the surface energy budget change through the uncertain cloud effect on shortwave radiation in boreal summer. The resulted uncertain change in summer surface heat flux alters the subsequent autumn and winter sea ice and contributes to significant differences in Arctic temperature via sea ice‐albedo feedback. This study suggests that internal uncertainty of an individual model is a non‐negligible source of overall uncertainty in simulating the MH Arctic temperature change.

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