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William A. Komaromi and James D. Doyle

13 km out to a radius of 100 km from high-resolution Weather Research and Forecasting (WRF) Model simulations, and demonstrate a reduction of I in the TC core and moat region along with an increase in I outside of the primary eyewall during secondary eyewall formation. However, they do not include the outflow region in their analyses. As is the case with outflow, the TC warm core has traditionally been infrequently documented by in situ observations because of its combination of high altitude

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