Scientists Find the Error Source of a Sea-ice Model Varies with the Season
Arctic sea ice has been rapidly declining in recent decades, and changes in arctic sea ice can have a significant impact on global weather and climate through interactions with the atmosphere and oceans. In addition, the Arctic shipping routes are a shortcut to connect the major countries in the Northern Hemisphere. The Arctic region is also rich in natural resources and biological resources. Simulation of the Arctic sea ice could provide valuable information for Arctic shipping as well as climate studies, and it is therefore urgent to evaluate the ability to simulate Arctic sea ice and diagnose the sources of simulation errors.
To address the issue of error source identification, Prof. ZHENG Fei and his team from the Institute of Atmospheric Physics at 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).
"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," says ZHENG. "Due to the uncertainty of the model, the model's insufficient response to the signal of atmospheric forcings, and the insufficient response to the ocean boundary signal, there were disagreements between the simulations and observations in both March and September."
Schematic diagram of the sea-ice simulation error sources of a regional configuration of MITgcm (Image by SUN Yue).
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 the Arctic sea ice in different seasons in future work.
Citation: Zheng, F., Y. Sun, Q. H. Yang, and L. J. Mu, 2020: Evaluation of Arctic sea-ice cover and thickness simulated by MITgcm. Adv. Atmos. Sci., https://doi.org/10.1007/s00376-020-9223-6.
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