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Climate changes, including sea level rise (SLR) and typhoon intensification (TI), have had widespread impacts on natural systems.
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Following the upgrade to typhoon status, intensification briefly slowed but continued soon thereafter.
Large-scale fields and inner-core processes relevant to the formation and intensification of Typhoon Fengshen (2008) were investigated by a set of global cloud-permitting (3.5-km mesh) simulations.
Large-scale fields and inner-core processes relevant to the formation and intensification of Typhoon Fengshen (2008) were examined by simulations using a global nonhydrostatic model with a cloud-permitting resolution.
The next day, Forrest reached typhoon status, and the intensification process accelerated.
The researchers showed that the intensification of typhoons making landfall occurred because warmer coastal seas provided more energy to growing storms, enabling their wind speeds to increase more rapidly.
Further intensification to typhoon-status occurred by August 29.
The structural change culminated in Longwang becoming an annular typhoon and prompted re-intensification.
This implies that the air-sea enthalpy fluxes within the inner core of a simulated typhoon were insufficient to simulate intensification and the maximum intensity of the typhoon.
A low-level circulation in the Coral Sea helped enhance westerly flow to its south, which developed into a tropical depression late on December 4 and a tropical storm early on December 5. Intensification continued, and typhoon strength was reached late on December 6.
Back in favorable conditions, the typhoon entered a phase of rapid intensification beginning six hours later.
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