Great Red Spot

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The Great Red Spot is an anticyclonic hypercane on the planet Jupiter, 22° south of the equator, which has lasted at least 340 years. The storm is large enough to be visible through Earth-based telescopes. It was first observed by Cassini around 1665.

This dramatic view of Jupiter's Great Red Spot and its surroundings was obtained by Voyager 1 on February 25, 1979, when the spacecraft was 5.7 million miles (9.2 million kilometers) from Jupiter. Cloud details as small as 100 miles (160 kilometers) across can be seen here. The colorful, wavy cloud pattern to the left of the Red Spot is a region of extraordinarily complex and variable wave motion. To give a sense of Jupiter's scale, the white oval storm directly below the Great Red Spot is approximately the same diameter as Earth. The storm is now joined by a new Red Spot Red Spot Jr..

The oval object rotates counterclockwise, with a period of ~6 days. The Great Red Spot's dimensions are ~24–40,000 km × 12–14,000 km. It is large enough to contain two or three planets of Earth size. The cloudtops of this storm are ~8 km above the surrounding cloudtops.

Storms such as this are not uncommon within the turbulent atmospheres of gas giants. Jupiter also has white ovals and brown ovals, which are lesser unnamed storms. White ovals tend to consist of relatively cool clouds within the upper atmosphere. Brown ovals are warmer and located within the "normal cloud layer". Such storms can last hours or centuries.

1 Color and Visibility
2 Longevity
3 Mechanics
4 References
5 External links

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Color and Visibility

It is not known exactly what causes the Great Red Spot's reddish color. Theories supported by laboratory experiments suppose that the color may be caused by any of "complex organic molecules, red phosphorus, or yet another sulfur compound" [1], but a consensus has yet to be reached.

The Great Red Spot varies greatly in prominence, from almost brick-red to pale salmon, or even white. In fact, the Spot occasionally "disappears", becoming evident only through the Red Spot Hollow, which is its niche in the South Equatorial Belt (SEB). Interestingly, its visibility is apparently coupled to the SEB; when the Belt is bright white, the Spot tends to be dark, and when it is dark the Spot is usually light. These periods when the Spot is dark or light occur at irregular intervals; in the last 50 years the Spot was darkest from 1961-66, 1968-75, 1989-90, and 1992-93.(Beebe 38-41)

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Longevity

The Great Red Spot appears at first to be remarkably stable, and most sources concur that it has been continuously observed for 300 years. However, the situation is more complex than that; the present Spot was first seen only in 1830, and well studied only after a prominent apparition in 1879. A long gap separates its period of current study after 1830 from its 17th century discovery; whether the original Spot dissipated and reformed, or whether it faded, or even if the observational record was simply poor are all unknown.(Beebe 38-41)

Several factors may be responsible for its longevity, such as the fact that it never encounters solid surfaces over which to dissipate its energy and that its motion is driven by Jupiter's internal heat. Simulations suggest that the Spot tends to absorb smaller atmospheric disturbances.

At the start of 2004, the Great Red Spot was approximately half as large as it was 100 years ago. It is not known how long the Great Red Spot will last, or whether this is a result of normal fluctuations.

The Great Red Spot should not be confused with the Great Dark Spot, famously seen in the atmosphere of Neptune by Voyager 2 in 1989. The Great Dark Spot may have been an atmospheric hole rather than a storm, and it is no longer present as of 1994 (although a similar spot had appeared farther to the north).

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Mechanics

As hot air rises from lower levels of Jupiter's atmosphere, eddies form and converge together. A Coriolis force forms and forces cooler air to fall back into a swirling motion that may be many kilometers in diameter. These eddies can last for a long time, because there is no solid surface to provide friction and colder cloud tops above the eddie allow little energy to escape by radiation. Once formed, such eddies are free to move, merging with or affecting the behaviour of other storm systems in the atmosphere. It is theorized that this mechanism formed the great red spot. According to this theory, many adjacent eddies are engulfed and merge with the spot, adding to the energy of the storm and contributing to its longevity.

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References

Beatty, Kelly J., Peterson, Carolyn Collins, Chaiki, Andrew. "The New Solar System". Massachusetts: Sky Publishing Corporation, 1999.
Beebe, Reta. "Jupiter The Giant Planet" Smithsonian Institution 1997.
Peek Bertrand M. "The Planet Jupiter". London: Faber and Faber Limited, 1981.
Rogers, John H. "The Giant Planet Jupiter". Cambridge: Press Syndicate of the University of Cambridge, 1995
Youssef, Ashraf, Marcus, Philip S. "The dynamics of jovian white ovals from formation to merger". 1 November 2000: 74-93.

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