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Lagrangian Analysis of Tropical Cyclone Intensification Simulated by General Circulation Models Compared with Observations


Fig. A1.

Climatology of environmental conditions constituting V6 calculated by the (left) Lagrangian and (right) Eulerian approaches obtained from the CNTL simulation. Note that the left column is identical to that in Fig. 9. As described in section 2c, environmental variables along the TC tracks are used for the Lagrangian approach. Monthly-averaged environmental variables during the TC seasons (i.e., July–October in the Northern Hemisphere and December–March in the Southern Hemisphere) are used for the Eulerian approach.

Citation: Journal of Climate 36, 24; 10.1175/JCLI-D-23-0070.1



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