Showing posts with label Jupiter’s atmosphere. Show all posts
Showing posts with label Jupiter’s atmosphere. Show all posts

Friday, March 19, 2021

Powerful stratospheric winds measured on Jupiter for the first time

Representation of stratospheric winds near Jupiter’s south pole
 
Comet Shoemaker–Levy 9 impacting Jupiter in 1994
 
Sharpening up Jupiter




Videos

Powerful stratospheric winds near Jupiter’s south pole (animation)
Powerful stratospheric winds near Jupiter’s south pole (animation) 
 
Animated view of Jupiter showing comet Shoemaker–Levy 9 impact sites
Animated view of Jupiter showing comet Shoemaker–Levy 9 impact sites



 

Using the Atacama Large Millimeter/submillimeter Array (ALMA), in which the European Southern Observatory (ESO) is a partner, a team of astronomers have directly measured winds in Jupiter’s middle atmosphere for the first time. By analysing the aftermath of a comet collision from the 1990s, the researchers have revealed incredibly powerful winds, with speeds of up to 1450 kilometres an hour, near Jupiter’s poles. They could represent what the team have described as a “unique meteorological beast in our Solar System”.

Jupiter is famous for its distinctive red and white bands: swirling clouds of moving gas that astronomers traditionally use to track winds in Jupiter’s lower atmosphere. Astronomers have also seen, near Jupiter's poles, the vivid glows known as aurorae, which appear to be associated with strong winds in the planet’s upper atmosphere. But until now, researchers had never been able to directly measure wind patterns in between these two atmospheric layers, in the stratosphere.

Measuring wind speeds in Jupiter’s stratosphere using cloud-tracking techniques is impossible because of the absence of clouds in this part of the atmosphere. However, astronomers were provided with an alternative measuring aid in the form of comet Shoemaker–Levy 9, which collided with the gas giant in spectacular fashion in 1994. This impact produced new molecules in Jupiter’s stratosphere, where they have been moving with the winds ever since. 

A team of astronomers, led by Thibault Cavalié of the Laboratoire d'Astrophysique de Bordeaux in France, have now tracked one of these molecules — hydrogen cyanide — to directly measure stratospheric "jets" on Jupiter. Scientists use the word "jets" to refer to narrow bands of wind in the atmosphere, like Earth’s jet streams.

"The most spectacular result is the presence of strong jets, with speeds of up to 400 metres per second, which are located under the aurorae near the poles," says Cavalié. These wind speeds, equivalent to about 1450 kilometres an hour, are more than twice the maximum storm speeds reached in Jupiter’s Great Red Spot and over three times the wind speed measured on Earth’s strongest tornadoes.

"Our detection indicates that these jets could behave like a giant vortex with a diameter of up to four times that of Earth, and some 900 kilometres in height," explains co-author Bilal Benmahi, also of the Laboratoire d’Astrophysique de Bordeaux. "A vortex of this size would be a unique meteorological beast in our Solar System," Cavalié adds.

Astronomers were aware of strong winds near Jupiter’s poles, but much higher up in the atmosphere, hundreds of kilometres above the focus area of the new study, which is published today in Astronomy & Astrophysics. Previous studies predicted that these upper-atmosphere winds would decrease in velocity and disappear well before reaching as deep as the stratosphere. "The new ALMA data tell us the contrary," says Cavalié, adding that finding these strong stratospheric winds near Jupiter’s poles was a "real surprise".

The team used 42 of ALMA’s 66 high-precision antennas, located in the Atacama Desert in northern Chile, to analyse the hydrogen cyanide molecules that have been moving around in Jupiter’s stratosphere since the impact of Shoemaker–Levy 9. The ALMA data allowed them to measure the Doppler shift — tiny changes in the frequency of the radiation emitted by the molecules — caused by the winds in this region of the planet. "By measuring this shift, we were able to deduce the speed of the winds much like one could deduce the speed of a passing train by the change in the frequency of the train whistle," explains study co-author Vincent Hue, a planetary scientist at the Southwest Research Institute in the US.

In addition to the surprising polar winds, the team also used ALMA to confirm the existence of strong stratospheric winds around the planet’s equator, by directly measuring their speed, also for the first time. The jets spotted in this part of the planet have average speeds of about 600 kilometres an hour.

The ALMA observations required to track stratospheric winds in both the poles and equator of Jupiter took less than 30 minutes of telescope time. "The high levels of detail we achieved in this short time really demonstrate the power of the ALMA observations," says Thomas Greathouse, a scientist at the Southwest Research Institute in the US and co-author of the study. "It is astounding to me to see the first direct measurement of these winds."

"These ALMA results open a new window for the study of Jupiter’s auroral regions, which was really unexpected just a few months back," says Cavalié. "They also set the stage for similar yet more extensive measurements to be made by the JUICE mission and its Submillimetre Wave Instrument," Greathouse adds, referring to the European Space Agency’s JUpiter ICy moons Explorer, which is expected to launch into space next year.

ESO’s ground-based Extremely Large Telescope (ELT), set to see first light later this decade, will also explore Jupiter. The telescope will be capable of making highly detailed observations of the planet’s aurorae, giving us further insight into Jupiter’s atmosphere.




More Information

This research is presented in the paper "First direct measurement of auroral and equatorial jets in the stratosphere of Jupiter" published today in Astronomy & Astrophysics (doi:10.1051/0004-6361/202140330).

The team is composed of T. Cavalié (Laboratoire d’Astrophysique de Bordeaux [LAB], France, and LESIA, Observatoire de Paris, PSL Research University [LESIA], France), B. Benmahi (LAB), V. Hue (Southwest Research Institute [SwRI], USA), R. Moreno (LESIA), E. Lellouch (LESIA), T. Fouchet (LESIA), P. Hartogh (Max-Planck-Institut für Sonnensystemforschung [MPS], Germany), L. Rezac (MPS), T. K. Greathouse (SwRI), G. R. Gladstone (SwRI), J. A. Sinclair (Jet Propulsion Laboratory, California Institute of Technology, USA), M. Dobrijevic (LAB), F. Billebaud (LAB) and C. Jarchow (MPS).

ESO is the foremost intergovernmental astronomy organisation in Europe and the world’s most productive ground-based astronomical observatory by far. It has 16 Member States: Austria, Belgium, the Czech Republic, Denmark, France, Finland, Germany, Ireland, Italy, the Netherlands, Poland, Portugal, Spain, Sweden, Switzerland and the United Kingdom, along with the host state of Chile and with Australia as a Strategic Partner. ESO carries out an ambitious programme focused on the design, construction and operation of powerful ground-based observing facilities enabling astronomers to make important scientific discoveries. ESO also plays a leading role in promoting and organising cooperation in astronomical research. ESO operates three unique world-class observing sites in Chile: La Silla, Paranal and Chajnantor. At Paranal, ESO operates the Very Large Telescope and its world-leading Very Large Telescope Interferometer as well as two survey telescopes, VISTA working in the infrared and the visible-light VLT Survey Telescope. Also at Paranal ESO will host and operate the Cherenkov Telescope Array South, the world’s largest and most sensitive gamma-ray observatory. ESO is also a major partner in two facilities on Chajnantor, APEX and ALMA, the largest astronomical project in existence. And on Cerro Armazones, close to Paranal, ESO is building the 39-metre Extremely Large Telescope, the ELT, which will become “the world’s biggest eye on the sky”.

The Atacama Large Millimeter/submillimeter Array (ALMA), an international astronomy facility, is a partnership of ESO, the U.S. National Science Foundation (NSF) and the National Institutes of Natural Sciences (NINS) of Japan in cooperation with the Republic of Chile. ALMA is funded by ESO on behalf of its Member States, by NSF in cooperation with the National Research Council of Canada (NRC) and the Ministry of Science and Technology (MOST) and by NINS in cooperation with the Academia Sinica (AS) in Taiwan and the Korea Astronomy and Space Science Institute (KASI). ALMA construction and operations are led by ESO on behalf of its Member States; by the National Radio Astronomy Observatory (NRAO), managed by Associated Universities, Inc. (AUI), on behalf of North America; and by the National Astronomical Observatory of Japan (NAOJ) on behalf of East Asia. The Joint ALMA Observatory (JAO) provides the unified leadership and management of the construction, commissioning and operation of ALMA.




Links

Thibault Cavalié
Laboratoire d'Astrophysique de Bordeaux
Bordeaux, France
Tel: +33 (0)5 40 00 32 71
Email:
thibault.cavalie@u-bordeaux.fr

Bilal Benmahi
Laboratoire d'Astrophysique de Bordeaux
Bordeaux, France
Tel: +33 (0)5 40 00 32 76
Email:
bilal.benmahi@u-bordeaux.fr

Vincent Hue
Southwest Research Institute
San Antonio, TX, USA
Tel: +1 (210) 522-5027
Email:
vhue@swri.org

Thomas Greathouse
Southwest Research Institute
San Antonio, TX, USA
Tel: +1 (210) 522-2809
Email:
tgreathouse@swri.edu

Suzanna Randall (astronomer who did not participate in the study; contact for external comment and questions on ALMA)
European Southern Observatory
Garching bei München, Germany
Email:
srandall@eso.org

Bárbara Ferreira
ESO Media Manager
Garching bei München, Germany
Tel: +49 89 3200 6670
Cell: +49 151 241 664 00
Email:
press@eso.org

 Source: ESO/News


Monday, December 16, 2019

Radio Jupiter: Seeing the Giant Planet in a New Light

Radio image of Jupiter made with ALMA. Bright bands indicate high temperatures and dark bands low temperatures. The dark bands correspond to the zones on Jupiter, which are often white at visible wavelengths. The bright bands correspond to the brown belts on the planet. This image contains over 10 hours of data, so fine details are smeared by the planet's rotation. Credit: ALMA (ESO/NAOJ/NRAO), I. de Pater et al.; NRAO/AUI NSF, S. Dagnello

Flat map of Jupiter in radio waves with ALMA (top) and visible light with the Hubble Space Telescope (bottom). The eruption in the South Equatorial Belt is visible in both images. Credit: ALMA (ESO/NAOJ/NRAO), I. de Pater et al.; NRAO/AUI NSF, S. Dagnello; NASA/Hubble. Hi-res image

Burke and Franklin's antenna array.
Credit: Carnegie Institution of Washington. Hi-res image

Radio image (bottom) captured by the VLA of Jupiter's Great Red Spot, compared with a visible-light image (top) from the Hubble Space Telescope. Credit: de Pater, et al., NRAO/AUI/NSF; NASA. Hi-res image

A 2003 image of Jupiter. The lobes on each side of the planet are caused by Jupiter's strong magnetosphere.
Credit: NRAO/AUI/NSF. Hi-res image



Jupiter is the largest planet in our solar system. It is also the brightest planet at radio frequencies. While radio astronomy often focuses on more distant objects such as nebulae and galaxies, the radio astronomy of planets begins with Jupiter.

While other planets in our solar system emit radio light, Jupiter is by far the most radio bright. When charged particles in space interact with Jupiter’s magnetic field, they emit radio light through a process known as synchrotron radiation. The first radio observation of Jupiter was made by Bernard Burke and Kenneth Franklin in 1955. They weren’t expecting such a signal, so they initially thought it was the radio noise of a farm-hand driving home. But subsequent observations showed the signal was Jovian in origin.

In addition to its synchrotron emissions, Jupiter also gives off radio light due to thermal emissions. These fainter emissions were first mapped by the Very Large Array (VLA). The VLA’s antennas can work together in a wide configuration to capture faint and high-resolution radio images.

When the VLA was upgraded in 2011, it greatly increased its sensitivity and imaging capabilities. In 2013 the VLA gathered the first radio images of Jupiter’s atmosphere. It allowed us to peer into Jupiter’s thick atmosphere. Observations in visible light are limited by the cloud layer of Jupiter. But radio light penetrates these cloud layers more easily. The VLA observations let us see 100 kilometers below the visible clouds. They captured details of the great red spot, and how ammonia within Jupiter’s cloud layer rises and falls.

Recently the Atacama Large Millimeter/submillimeter Array (ALMA) also captured even higher resolution images of Jupiter’s thermal emissions. ALMA operates at shorter wavelengths than the VLA. Since shorter wavelengths are absorbed more readily by Jupiter’s atmosphere, ALMA’s observation only penetrates about 50 kilometers below Jupiter’s cloud layer. But ALMA’s high resolution allowed astronomers to create a three-dimensional map of ammonia gas within the atmosphere. This helps us understand the mechanisms that drive storms on Jupiter.

As radio technology has advanced, the radio astronomy of Jupiter has become much more accessible. With only modest radio equipment, you can observe the radio light of Jupiter for yourselves. Projects such as NASA’s Radio JOVE encourage students and amateur scientists to observe radio emissions from Jupiter and other bright radio sources. The project teaches students about radio astronomy and engages in citizen science research projects.

Jupiter has long inspired humanity to look toward the stars. From Galileo’s first view through his telescope, to the radio arrays of the VLA and ALMA, the light of Jupiter at all wavelengths has much to offer.




Reference: de Pater, Imke, et al. “Peering through Jupiter’s clouds with radio spectral imaging.” Science 352.6290 (2016): 1198-1201.

Reference: de Pater, Imke, et al. “First ALMA Millimeter-wavelength Maps of Jupiter, with a Multiwavelength Study of Convection.” The Astronomical Journal 158.4 (2019): 139.