Predictability Associated with the Downstream Impacts of the Extratropical Transition (ET) of Tropical Cyclones
Abstract
The poleward movement of a
decaying tropical cyclone (TC) often results
in a rapidly-moving, explosively-deepening
midlatitude cyclone. The re-intensification of
the remnant TC as an extratropical cyclone
depends on the phasing between the
decaying TC and a midlatitude environment
that is favorable for midlatitude
cyclogenesis.
Description
P6.7