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By July 15, the storm attained its peak strength as a Category 5 equivalent super typhoon with winds estimated at 260 km/h (160 mph).
At the end of this phase, Gordon attained its peak strength as a Category 5 equivalent super typhoon with winds estimated at 260 km/h (160 mph).
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A recently presented single plastic-potential, microstructure-based model of poly-crystal plasticity by the authors considers a globally regularized Schmid law (RSL) as the slip flow criterion of a homogeneous equivalent super-crystal.
Estimates from the Joint Typhoon Warning Center ranked the system as a Category 5-equivalent super typhoon with one-minute sustained winds of 260 km/h (160 mph), though this is argued to have underrepresented the typhoon's strength.
Early on September 15, the JTWC reported that Typhoon Choi-wan had intensified further and had become a Category 4-equivalent Super Typhoon whilst passing over the island of Alamagan.
The JTWC estimated Cimaron to have been a stronger system, attaining its peak intensity as a Category 5-equivalent super typhoon with one-minute winds of 260 km/h (160 mph).
The JTWC estimated Saomai to have been a much more powerful system, ranking it as a Category 5-equivalent super typhoon with one-minute winds of and a pressure of 898 mbar (hPa; 26.52 inHg).
Karen became a tropical storm late on November 7, and within two days it explosively intensified into a Category 5-equivalent super typhoon on the Saffir Simpson hurricane scale.
By the evening of October 5, Nora had attained winds in excess of 260 km/h (160 mph), ranking it as a Category 5-equivalent super typhoon on the Saffir Simpson hurricane scale.
At the end of this phase, Karen featured an 8-10 km wide eye and had estimated surface winds of 295 km/h (185 mph), ranking it as a modern day Category 5-equivalent super typhoon on the Saffir Simpson hurricane scale.
Typhoon Choi-wan was a powerful typhoon that became the first Category 5 equivalent-super typhoon to form during the 2009 Pacific typhoon season.
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