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With warm waters and a favorable upper level environment, the depression quickly re-intensified as convection increased.
The upper level environment ahead of the storm was very favorable, and the oceanic heat content was very high.
Flora remained a hurricane while drifting over land due to abundant moisture and a favorable upper level environment.
Due to a favorable upper level environment, forecasters predicted the depression to intensify to a 70 mph (110 km/h) tropical storm after making landfall on Haiti and eastern Cuba.
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The upper-level environment rapidly changed, and the cyclones convection became disorganized.
It was located over very warm water temperatures, although the upper-level environment was not conducive for significant intensification.
A shortwave trough located over the Korean peninsula provided a favorable upper-level environment for Faxai to intensify.
Water temperatures were slightly warmer than usual, and there was a favorable upper-level environment for strengthening.
Although the system was located over warmer than average sea surface temperatures, the upper-level environment was initially unfavorable.
Its favorable upper-level environment allowed the outflow to become better defined, with a large eye and nearby dry air being the primary restraining factors for development.
However, the upper-level environment gradually became more favorable for further development, and deep convection, or thunderstorm activity, developed closer to the center.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com