Measurement and implications of Saturn’s gravity field and ring mass
The interior structure of Saturn, the depth of its winds, and the mass and age of its rings constrain its formation and evolution. In the final phase of the Cassini mission, the spacecraft dived between the planet and its innermost ring, at altitudes of 2600 to 3900 kilometers above the cloud tops....
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 2019-06, Vol.364 (6445), p.1052-1052 |
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creator | Iess, L. Militzer, B. Kaspi, Y. Nicholson, P. Durante, D. Racioppa, P. Anabtawi, A. Galanti, E. Hubbard, W. Mariani, M. J. Tortora, P. Wahl, S. Zannoni, M. |
description | The interior structure of Saturn, the depth of its winds, and the mass and age of its rings constrain its formation and evolution. In the final phase of the Cassini mission, the spacecraft dived between the planet and its innermost ring, at altitudes of 2600 to 3900 kilometers above the cloud tops. During six of these crossings, a radio link with Earth was monitored to determine the gravitational field of the planet and the mass of its rings. We find that Saturn's gravity deviates from theoretical expectations and requires differential rotation of the atmosphere extending to a depth of at least 9000 kilometers. The total mass of the rings is (1.54 ± 0.49) × 10
kilograms (0.41 ± 0.13 times that of the moon Mimas), indicating that the rings may have formed 10
to 10
years ago. |
doi_str_mv | 10.1126/science.aat2965 |
format | Article |
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kilograms (0.41 ± 0.13 times that of the moon Mimas), indicating that the rings may have formed 10
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kilograms (0.41 ± 0.13 times that of the moon Mimas), indicating that the rings may have formed 10
to 10
years ago.</description><subject>Age</subject><subject>Angular velocity</subject><subject>Astronomy</subject><subject>Atmosphere</subject><subject>Atmospheric models</subject><subject>Cassini mission</subject><subject>Catastrophic events</subject><subject>Centrifugal force</subject><subject>Clouds</subject><subject>Deposition</subject><subject>Earth</subject><subject>Equator</subject><subject>Evolution</subject><subject>Flow profiles</subject><subject>Free fall</subject><subject>Gravitation</subject><subject>Gravitational fields</subject><subject>Gravity</subject><subject>Jupiter</subject><subject>Jupiter atmosphere</subject><subject>Mass distribution</subject><subject>Moon</subject><subject>Moons</subject><subject>Optical tracking</subject><subject>Orbits</subject><subject>Outer solar system</subject><subject>Planetary rotation</subject><subject>Planets</subject><subject>Radial velocity</subject><subject>RESEARCH ARTICLE SUMMARY</subject><subject>Saturn</subject><subject>Saturn atmosphere</subject><subject>Solar system</subject><subject>Spacecraft</subject><subject>Stellar winds</subject><subject>Velocity</subject><subject>Velocity distribution</subject><issn>0036-8075</issn><issn>1095-9203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNpdkL1OwzAURi0EoqUwM4EisbCktePYjkdUUUAqYgDmyHGuK1f5KXaC1I3X4PV4EgwNHZjucM_36d6D0DnBU0ISPvPaQqNhqlSXSM4O0JhgyWKZYHqIxhhTHmdYsBE68X6NcdhJeoxGFHPG0lSM0eIRlO8d1NB0kWrKyNabymrV2bbxUWuiZ9X1rvn6-PTRyql3220jY6Eqf2Fnm1VUK-9P0ZFRlYezYU7Q6-L2ZX4fL5_uHuY3y1ilQnSx1KC5MYZKrUvgDJgGWQAniulCAOZCFmWWMiykxIyIlDNtZKaINJlQHNMJut71blz71oPv8tp6DVWlGmh7nydEyBQnIRzQq3_oug2fhOvyJKFSZKGdBmq2o7RrvXdg8o2ztXLbnOD8R3E-KM4HxSFxOfT2RQ3lnv9zGoCLHbD2Xev2-4TzjDDB6TdowoPn</recordid><startdate>20190614</startdate><enddate>20190614</enddate><creator>Iess, L.</creator><creator>Militzer, B.</creator><creator>Kaspi, Y.</creator><creator>Nicholson, P.</creator><creator>Durante, D.</creator><creator>Racioppa, P.</creator><creator>Anabtawi, A.</creator><creator>Galanti, E.</creator><creator>Hubbard, W.</creator><creator>Mariani, M. 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J.</au><au>Tortora, P.</au><au>Wahl, S.</au><au>Zannoni, M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Measurement and implications of Saturn’s gravity field and ring mass</atitle><jtitle>Science (American Association for the Advancement of Science)</jtitle><addtitle>Science</addtitle><date>2019-06-14</date><risdate>2019</risdate><volume>364</volume><issue>6445</issue><spage>1052</spage><epage>1052</epage><pages>1052-1052</pages><issn>0036-8075</issn><eissn>1095-9203</eissn><abstract>The interior structure of Saturn, the depth of its winds, and the mass and age of its rings constrain its formation and evolution. In the final phase of the Cassini mission, the spacecraft dived between the planet and its innermost ring, at altitudes of 2600 to 3900 kilometers above the cloud tops. During six of these crossings, a radio link with Earth was monitored to determine the gravitational field of the planet and the mass of its rings. We find that Saturn's gravity deviates from theoretical expectations and requires differential rotation of the atmosphere extending to a depth of at least 9000 kilometers. The total mass of the rings is (1.54 ± 0.49) × 10
kilograms (0.41 ± 0.13 times that of the moon Mimas), indicating that the rings may have formed 10
to 10
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subjects | Age Angular velocity Astronomy Atmosphere Atmospheric models Cassini mission Catastrophic events Centrifugal force Clouds Deposition Earth Equator Evolution Flow profiles Free fall Gravitation Gravitational fields Gravity Jupiter Jupiter atmosphere Mass distribution Moon Moons Optical tracking Orbits Outer solar system Planetary rotation Planets Radial velocity RESEARCH ARTICLE SUMMARY Saturn Saturn atmosphere Solar system Spacecraft Stellar winds Velocity Velocity distribution |
title | Measurement and implications of Saturn’s gravity field and ring mass |
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