Gamma ray

The maximum potential intensity of a tropical cyclone is the theoretical limit of the strength of a tropical cyclone. It is computed using the following formula:

$V=A+B\cdot e^{C(T-T_0)}$

Where $V$ is the maximum potential velocity in meters per second; $T$ is the sea surface temperature underneath the center of the tropical cyclone, $T_0$ is a reference temperature (30 ˚C) and $A$, $B$ and $C$ are curve-fit constants. When $A=28.2$, $B=55.8$, and $C=0.1813$, the graph generated by this function corresponds to the 99th percentile of empirical tropical cyclone intensity data.

References

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External links

• Alternate MPI calculation
• MPI climatology
• Real-time maps of maximum potential intensity worldwide

Hello, I'm Willard, a 30 year old from Capodimonte, Italy.
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