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Hypercane

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A hypercane is a hypothetical class of extreme tropical cyclone that could form if sea surface temperatures reached approximately 50 °C (122 °F), which is 12 °C (22 °F) warmer than the warmest ocean temperature ever recorded.[1] 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.[2] 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.[3] The hypothesis was created by Kerry Emanuel of MIT, who also coined the term.[4][5][3]

Description[edit]

The relative sizes of Typhoon Tip, Cyclone Tracy, and the Contiguous United States. While the average hypercane would not exceed Cyclone Tracy in size, the largest hypercanes could exceed even Typhoon Tip in size.

In order to form a hypercane, according to Emanuel's hypothetical model, the ocean temperature would have to be at least 49 °C (120 °F). 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.[6]

Hypercanes would have wind speeds of over 800 kilometres per hour (500 mph), potentially gusting to 970 km/h (600 mph),[7] and would also have a central pressure of less than 700 hectopascals (20.67 inHg), giving them an enormous lifespan of at least several weeks.[5] The pressure drop, compared to mean sea level pressure, would be the equivalent of being at almost 3,000 m (or about 10,000 ft) in elevation,[8] a level sufficient to cause altitude sickness.[9] This extreme low pressure could also support massive storm systems roughly the size of North America.[5][10] For comparison, the largest and most intense storm on record was 1979's Typhoon Tip, with a 1-minute sustained wind speed of 305 km/h (190 mph) and a minimum central pressure of 870 hPa (25.69 inHg). 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 345 km/h (215 mph).[11] However, hypercanes may be as small as 25 km (15 mi) in size, and they would lose strength quickly after venturing into colder waters.[7]

The waters after a hypercane could remain hot enough for weeks, allowing more hypercanes to form. A hypercane's clouds would reach 30 to 40 km (20 to 25 mi) into the stratosphere. Such an intense storm would also damage the Earth's ozone layer, potentially having devastating consequences for life on Earth.[5][failed verification] Water molecules in the stratosphere would react with ozone to accelerate decay into O2 and reduce absorption of ultraviolet light.[12]

Mechanism[edit]

A hurricane functions 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. [citation needed]

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.[3][13]

See also[edit]

References[edit]

  1. ^ "Temperature of Ocean Water". Windows to the Universe. University Corporation for Atmospheric Research. August 31, 2001. Archived from the original on March 13, 2012. Retrieved July 24, 2008.
  2. ^ Leahy, Stephen (September 16, 2005). "The Dawn of the Hypercane?". Inter Press Service. Archived from the original on May 17, 2008. Retrieved July 24, 2008.
  3. ^ Jump up to: a b c Emanuel, Kerry; Speer, Kevin; Rotunno, Richard; Srivastava, Ramesh; Molina, Mario (July 20, 1995). "Hypercanes: A Possible Link to Global Extinction Scenarios". Journal of Geophysical Research. 100 (D7): 13755–13765. Bibcode:1995JGR...10013755E. doi:10.1029/95JD01368. Archived from the original on October 2, 2012. Retrieved July 24, 2008.
  4. ^ Hecht, Jeff (February 4, 1995). "Did storms land the dinosaurs in hot water?". New Scientist. No. 1963. p. 16. Retrieved July 24, 2008.
  5. ^ Jump up to: a b c d Emanuel, Kerry (September 16, 1996). "Limits on Hurricane Intensity". Center for Meteorology and Physical Oceanography, MIT. Retrieved July 24, 2008.
  6. ^ Emanuel, Kerry (2008). "Hypercane". Mega Disasters (Interview). History Channel.
  7. ^ Jump up to: a b Michael Cabbage (September 10, 1997). "'HYPERCANE' THEORY PACKS 600 MPH WINDS". South Florida Sun Sentinel. Archived from the original on May 13, 2019. Retrieved May 13, 2019.
  8. ^ "Altitude to Pressure Conversion Table". SensorsONE. May 22, 2024. Retrieved May 23, 2024.
  9. ^ "Travel to High Altitudes". CDC. September 14, 2020. Retrieved May 24, 2024.
  10. ^ Jhaneel Lockhart (2017). "Could a 500 Mph "Hypercane" End Life As We Know It?". Roaring Earth. Retrieved March 13, 2021.
  11. ^ Henson, Robert (2008). "Hypercane". Mega Disasters (Interview). History Channel.
  12. ^ "ozone decomposition". www.lenntech.com. Retrieved February 5, 2019.
  13. ^ Emanuel, Kerry A. (1988). "The Maximum Intensity of Hurricanes". Journal of the Atmospheric Sciences. 45 (7): 1143–1155. Bibcode:1988JAtS...45.1143E. doi:10.1175/1520-0469(1988)045<1143:TMIOH>2.0.CO;2.

External links[edit]

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