Tropical cyclones derive their energy from the warm waters of the ocean, which provide the latent heat necessary for the formation and intensification of the storm.

The eye of a tropical cyclone is the central region of calm weather, surrounded by the storm's strongest winds and heaviest rainfall.

Cyclonic circulation refers to the inward spiraling of winds around the center of a tropical cyclone, which is caused by the pressure gradient between the low pressure at the center and the higher pressure outside the storm.

Blizzards are characterized by heavy snowfall and strong winds, and are not associated with tropical cyclones.

The Saffir-Simpson Hurricane Wind Scale is used to classify the intensity of hurricanes based on their maximum sustained wind speeds, with categories ranging from 1 to 5.

Inundation refers to the flooding of coastal areas caused by the storm surge, which is a dome of water pushed ashore by the strong winds of a tropical cyclone.

Droughts are not typically associated with tropical cyclones, which are characterized by heavy rainfall and flooding.

Extratropical transition is the process by which a tropical cyclone loses its tropical characteristics and becomes a mid-latitude cyclone, typically as it moves away from warm tropical waters.

The Mediterranean Sea is not typically affected by tropical cyclones due to its relatively small size and enclosed nature.

Rainbands are the spiral-shaped bands of clouds and thunderstorms that extend outward from the center of a tropical cyclone, bringing heavy rainfall.

Strong vertical wind shear, which is a difference in wind speed and direction with height, can disrupt the formation and development of tropical cyclones.

Cyclogenesis refers to the process of tropical cyclone formation and intensification, which involves the organization of thunderstorms around a low-pressure center over warm ocean waters.

Wildfires are not typically associated with tropical cyclones, which are characterized by heavy rainfall and flooding.

Peak winds refer to the maximum sustained wind speeds of a tropical cyclone, which are typically measured at a height of 10 meters above the surface.

The Arctic Ocean is not typically affected by tropical cyclones due to its cold temperatures and lack of warm ocean waters.