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土星低纬度平流层温度的半年振荡。

Semi-annual oscillations in Saturn's low-latitude stratospheric temperatures.

作者信息

Orton Glenn S, Yanamandra-Fisher Padma A, Fisher Brendan M, Friedson A James, Parrish Paul D, Nelson Jesse F, Bauermeister Amber Swenson, Fletcher Leigh, Gezari Daniel Y, Varosi Frank, Tokunaga Alan T, Caldwell John, Baines Kevin H, Hora Joseph L, Ressler Michael E, Fujiyoshi Takuya, Fuse Tetsuharu, Hagopian Hagop, Martin Terry Z, Bergstralh Jay T, Howett Carly, Hoffmann William F, Deutsch Lynne K, Van Cleve Jeffrey E, Noe Eldar, Adams Joseph D, Kassis Marc, Tollestrup Eric

机构信息

MS 169-237, Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, California 91109, USA.

出版信息

Nature. 2008 May 8;453(7192):196-9. doi: 10.1038/nature06897.

Abstract

Observations of oscillations of temperature and wind in planetary atmospheres provide a means of generalizing models for atmospheric dynamics in a diverse set of planets in the Solar System and elsewhere. An equatorial oscillation similar to one in the Earth's atmosphere has been discovered in Jupiter. Here we report the existence of similar oscillations in Saturn's atmosphere, from an analysis of over two decades of spatially resolved observations of its 7.8-microm methane and 12.2-microm ethane stratospheric emissions, where we compare zonal-mean stratospheric brightness temperatures at planetographic latitudes of 3.6 degrees and 15.5 degrees in both the northern and the southern hemispheres. These results support the interpretation of vertical and meridional variability of temperatures in Saturn's stratosphere as a manifestation of a wave phenomenon similar to that on the Earth and in Jupiter. The period of this oscillation is 14.8 +/- 1.2 terrestrial years, roughly half of Saturn's year, suggesting the influence of seasonal forcing, as is the case with the Earth's semi-annual oscillation.

摘要

对行星大气中温度和风振荡的观测提供了一种方法,可用于推广太阳系及其他地方各种行星大气动力学的模型。在木星上发现了一种类似于地球大气中的赤道振荡。在此,我们通过对土星大气中20多年来7.8微米甲烷和12.2微米乙烷平流层发射的空间分辨观测进行分析,报告了土星大气中类似振荡的存在,我们比较了南北半球行星地理纬度3.6度和15.5度处的纬向平均平流层亮度温度。这些结果支持将土星平流层温度的垂直和经向变化解释为一种类似于地球和木星上的波动现象的表现。这种振荡的周期为14.8±1.2地球年,大约是土星一年的一半,这表明存在季节性强迫的影响,就像地球的半年振荡一样。

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