Research Article
Periodic Cycles of Eyewall Convection Limit the Rapid Intensification of Typhoon Hato (2017)
Figure 14
Variation of the azimuthally averaged remaining thermodynamic terms of LH from vertical advection except (−()/(Cpd)·∂q/∂z in equation (2); shading) with the radius and height of (vectors). (a, c, e) The velocities with absolute values above the threshold defined in Section 3.3. (b, d, f) The velocities with absolute values below the threshold.
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