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Space Topics: Venus

Views of Venus' South Pole from Venus Express

Venus Express entered orbit at Venus on April 11, 2006. Its first orbit was a highly elliptical one that carried it to a distance of 350,000 kilometers from the planet's south pole, permitting the spacecraft essentially to "park" over the pole for several days. From that point of view it observed a south polar vortex structure similar to the north polar one that had been studied by Mariner 10 and Pioneer Venus in the 1970s and 1980s.

Venus Express carries a Visible and Infrared Thermal Imaging Spectrometer that can capture images penetrating to different levels within Venus' clouds, depending upon the choice of wavelength. Venus' thick atmosphere has many different cloud layers, and understanding this vertical structure is one of the goals of the Venus Express mission.

First images from Venus Express VIRTIS
First images from Venus Express VIRTIS
These false-color views of the south pole of Venus were captured as part of a single observation by the VIRTIS imaging spectrometer on April 12, 2006. The left half is a day-side view composed of ultraviolet and infrared images and shows swirling clouds at an altitude of 70 to 80 kilometers above the surface. The right half shows heat being emanated from the surface on Venus' night side. Wispy, opaque clouds at an atltitude of about 50 kilometers block the thermal energy from escaping Venus, so the image is in effect a backlit view of the 50-kilometer-altitude clouds. Credit: ESA / INAF-IASF, Rome, Italy, and Obs. de Paris, France

The images below were captured over a period of a week in three different wavelengths:

  • Ultraviolet/visible (380 nanometers): At this wavelength, only the day side of Venus is visible where its uppermost clouds at an elevation of 80 kilometers (50 miles) reflect incoming sunlight. Wispy cloud features are visible.
  • Near infrared (1.7 microns): At this wavelength, clouds floating at elevations of about 20 to 30 kilometers (12 to 18 miles) block thermal radiation that is emitted from lower in the atmosphere. The clouds are dark; windows through the clouds are bright.
  • Thermal infrared (5 microns): At this wavelength, heat emitted from the upper part of the atmosphere at elevations of 60-80 kilometers (35 to 50 miles) is visible. A polar "dipole" feature rotates exactly at the south pole.
Venus' south pole
Venus' south pole
April 12, 2006
Range: 210,000 kilometers
Venus' south pole
Venus' south pole
April 13, 2006
Range: 280,000 kilometers
Venus' south pole
Venus' south pole
April 14, 2006
Range: 315,000 kilometers
Venus' south pole
Venus' south pole
April 16, 2006
Range: 315,000 kilometers
Venus' south pole
Venus' south pole
April 17, 2006
Range: 270,000 kilometers
Venus' south pole
Venus' south pole
April 19, 2006
Range: 190,000 kilometers
All images credit: ESA / VIRTIS / INAF-IASF / Obs. de Paris-LESIA
A week of weather over Venus' south pole
A week of weather over Venus' south pole
This animation is made of the 5-micron data (orange-tinted images above), reprojected so that the south pole stays at the center of the image. The polar vortex shows up as an unusually warm feature at the south pole, surrounded by a collar of colder air. Credit: ESA / VIRTIS / INAF-IASF / Obs. de Paris-LESIA