Hypercane. A hypercane is a hypothetical class of extreme tropical cyclone that could form if sea surface temperatures reached approximately , which is  warmer than the warmest ocean temperature ever recorded. Such an increase could be caused by a large asteroid or comet impact, a large supervolcanic eruption, a large submarine flood basalt, or "incredible" global warming. There is some speculation that a series of hypercanes resulting from the impact of a large asteroid or comet contributed to the demise of the non-avian dinosaurs. The hypothesis was created by Kerry Emanuel of MIT, who also coined the term.

Description

In order to form a hypercane, according to Emanuel's hypothetical model, the ocean temperature would have to be at least . A critical difference between a hypercane and present-day hurricanes is that a hypercane would extend into the upper stratosphere, whereas present-day hurricanes extend into only the lower stratosphere.

Hypercanes would have wind speeds of over , potentially gusting to , and would also have a central pressure of less than , giving them an enormous lifespan of at least several weeks. The pressure drop, compared to mean sea level pressure, would be the equivalent of being at almost  in elevation, a level sufficient to cause altitude sickness. This extreme low pressure could also support massive storm systems roughly the size of North America. For comparison, the largest and most intense storm on record was 1979's Typhoon Tip, with a 1-minute sustained wind speed of  and a minimum central pressure of . Such a storm would be nearly eight times more powerful than Hurricane Patricia, the storm with the highest sustained wind speed recorded, which had 1-minute sustained winds of . However, hypercanes may be as small as  in size, and they would lose strength quickly after venturing into colder waters.

The waters after a hypercane could remain hot enough for weeks, allowing more hypercanes to form. A hypercane's clouds would reach  into the stratosphere. Such an intense storm would also damage the Earth's ozone layer, potentially having devastating consequences for life on Earth. Water molecules in the stratosphere would react with ozone to accelerate decay into O2 and reduce absorption of ultraviolet light.

Mechanism
A hurricane can be idealized as a Carnot heat engine powered by the temperature difference between the sea and the uppermost layer of the troposphere. As air is drawn in towards the eye it acquires latent heat from evaporating sea-water, which is then released as sensible heat during the rise inside the eyewall and radiated away at the top of the storm system. The energy input is balanced by energy dissipation in a turbulent boundary layer close to the surface, which leads to an energy balance equilibrium. 

In Emanuel's model, if the temperature difference between the sea and the top of the troposphere is too large, there is no solution to the equilibrium equation. As more air is drawn in, the released heat reduces the central pressure further, drawing in more heat in a runaway positive feedback. The actual limit to hypercane intensity depends on other energy dissipation factors that are uncertain: whether inflow ceases to be isothermal, whether shock waves would form in the outflow around the eye, or whether turbulent breakdown of the vortex happens.

See also

 Global catastrophic risk
 Saffir–Simpson scale
 Tornado
 Extraterrestrial cyclone
 Great Red Spot
 Great Dark Spot

References

External links
 Hypercanes: The Next Big Disaster Movie? – YouTube

Tropical cyclone meteorology
Weather hazards
Doomsday scenarios
Geological hazards
Future problems
Meteorological hypotheses