An objective method is developed to identify concentric eyewalls (CEs) for typhoons using passive microwave satellite imagery from 1997 to 2011 in the western North Pacific basin.Three CE types are identified:CE with an eyewall replacement cycle (ERC; 37 cases),CE with no replacement cycle (NRC; 17 cases),and CE is maintained for an extended period (CEM; 16 eases).The inner eyewall (outer eyewall) of the ERC (NRC) type dissipates within 20 h after CE formation.The CEM type has its CE structure maintained for more than 20 h (mean duration time is 31 h).
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