Arctic sea-ice has been rapidly declining in recent decades, which can exert significant impacts on global weather and climate through interactions with the atmosphere and oceans. In addition, the Arctic shipping routes are a shortcut to connect major countries in the Northern Hemisphere. The Arctic region is also rich in natural resources and biological resources.
Simulation of the Arctic sea-ice can provide valuable information for Arctic shipping as well as climate studies. Therefore, it is urgent to evaluate the ability to simulate Arctic sea-ice and diagnose the sources of simulation errors.
A research team led by Prof. ZHENG Fei from the Institute of Atmospheric Physics (IAP) of the Chinese Academy of Sciences evaluated the sea-ice simulations of the Arctic regional ocean-ice coupling configuration of the Massachusetts Institute of Technology general circulation model (MITgcm) to address the issue of error source identification.
"We evaluated the model's performance in the Arctic cold season (March) and warm season (September), and found the model performances are different in the two months," said Prof. ZHENG. "Due to the uncertainty of the model, the model's insufficient response to the signal of atmospheric forcing, and the insufficient response to the ocean boundary signal, there were disagreements between the simulations and observations in both March and September."
According to their paper published in Advances in Atmospheric Sciences, the characteristics of seasonally varying model error sources could be fully considered by means of an ensemble approach, so as to achieve the goal of improving the simulation and prediction of Arctic sea-ice in different seasons in future work.
Schematic diagram of the sea-ice simulation error sources of a regional configuration of MITgcm (Image by SUN Yue)
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