Assimilation of satellite-retrieved sea ice concentration and prospects for september predictions of Arctic sea ice

The current GFDL seasonal prediction system achieved retrospective sea ice extent (SIE) skill without direct sea ice data assimilation. Here we develop sea ice data assimilation, shown to be a key source of skill for seasonal sea ice predictions, in GFDL's next-generation prediction system, the...

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Bibliographic Details
Published in:Journal of Climate
Other Authors: Zhang, Yong-Fei (author), Bushuk, Mitchell (author), Winton, Michael (author), Hurlin, Bill (author), Yang, Xiaosong (author), Delworth, Tom (author), Jia, Liwei (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Arctic
Sea ice
Online Access:https://doi.org/10.1175/JCLI-D-20-0469.1
Description
Summary:The current GFDL seasonal prediction system achieved retrospective sea ice extent (SIE) skill without direct sea ice data assimilation. Here we develop sea ice data assimilation, shown to be a key source of skill for seasonal sea ice predictions, in GFDL's next-generation prediction system, the Seamless System for Prediction and Earth System Research (SPEAR). Satellite sea ice concentration (SIC) observations are assimilated into the GFDL Sea Ice Simulator version 2 (SIS2) using the ensemble adjustment Kalman filter (EAKF). Sea ice physics is perturbed to form an ensemble of ice-ocean members with atmospheric forcing from the JRA-55 reanalysis. Assimilation is performed every 5 days from 1982 to 2017 and the evaluation is conducted at pan-Arctic and regional scales over the same period. To mitigate an assimilation overshoot problem and improve the analysis, sea surface temperatures (SSTs) are restored to the daily Optimum Interpolation Sea Surface Temperature version 2 (OISSTv2). The combination of SIC assimilation and SST restoring reduces analysis errors to the observational error level (similar to 10%) from up to 3 times larger than this (similar to 30%) in the free-running model. Sensitivity experiments show that the choice of assimilation localization half-width (190 km) is near optimal and that SIC analysis errors can be further reduced slightly either by reducing the observational error or by increasing the assimilation frequency from every 5 days to daily. A lagged-correlation analysis suggests substantial prediction skill improvements from SIC initialization at lead times of less than 2 months.

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