The cloud pattern on Jupiter is the visible system of colored cloud tops in the atmosphere of the planet Jupiter, remarkable for its stability. Astronomers have given names to parts of this pattern, using the word zone for the light stripes, and belt for the dark stripes, along various latitudes. The pattern and intensity of its belts and zones are famously variable, often changing markedly from opposition to opposition.


There are six major belts on Jupiter:

  • North and South Equatorial belts
  • North and South Temperate belts
  • N. North and S. South Temperate belts

There are seven major zones:

  • Equatorial zone
  • North and South Tropical zone
  • North and South Temperate zone
  • N. North and S. South Temperate zone

There are two polar regions:

  • South polar region
  • North polar region

Additionally, there are zones and belts that are more transient in nature and not always visible:

  • Equatorial belt
  • North Equatorial belt zone (a white zone within the belt)
  • South Equatorial belt zone
  • North Tropical zone belt (an additional belt inside the white zone)


The colored bands in Jupiter's clouds are caused as different-colored layers of clouds become visible.


Jupiter's clouds are made up of three different layers, growing colder as they increase in altitude:


The layer of ammonium hydrosulfide should be white. It is possible that impurities cause the reddish-brown color.

Circulation Cells

Jupiter, like most planets with atmospheres in the solar system, has multiple circulation cells, caused by the Coriolis effect, which occurs when a planet with a thick atmosphere spins rapidly. This causes warm air moving away from the equator of the planet and cold air moving away from the poles to become divided into east-west air currents. Jupiter has a particularly strong Coriolis Effect, due to its dense atmosphere and fast rotation, with winds reaching over 400 km/h. This also results in a greater number of circulation cells, compared to Earth's three.

Rising Gases

Jupiter's core is much hotter than the outer parts of its atmosphere. This causes the gases in its atmosphere to rise, cooling as they go. As they reach the altitude at which they can condense, they do so, while gases that condense at lower temperatures continue to rise. Eventually, the ammonia in the highest level of the clouds crystalizes, like snowflakes, causing the white clouds to disappear, allowing the darker ones below to become visible. Since each circulation cell is a different temperature, the different colors are arranged into bands.


The Great Red Spot is a storm feature on the border to the South Equatorial belt and has been observed for at least 300 years.

A feature in the South Temperate Belt, Oval BA, was first seen in 2000 after the collision of three small white storms, and has since appeared to have intensified. It is now approximately half the size of the Great Red Spot, and is starting to turn red. As a result, some scientists have begun calling it "Red Jr." [1]

There are always many smaller storms: brown, low pressure storms, and white, high pressure storms.


The normal pattern of bands and zones are sometimes disrupted for a period of time, and Astronomers call these events "Disturbances". For example, the longest lived disturbance in recorded history was a "Southern Tropical Disturbance" (STropD) from 1901 until 1939, discovered by Percy B. Molesworth on February 28, 1901. It created a darkened feature over some longitude area in the normally bright Southern Tropical zone.


  1. Bennett, Jeffrey; Donahue, Megan; Schneider, Nicholas; & Voit, Mark (2004). The Solar System: The Cosmic Perspective, (3rd ed.). San Francisco: Pearson Education, Inc. ISBN 0-8053-8930-X
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