土星上的一次季节变化英文原文
译:Jack


    土星远离太阳系的中心,在那儿,像一个巨大的飞碟的土星将自己“装扮成”行星的样子。土星那美丽的光环,随着土星绕太阳的公转,向以29年为一个周期我们“点头致意”着。这些是哈勃太空望远镜从1996年到2000年拍摄出来土星的照片。它们向我们展示了土星的光环正慢慢地张开的过程:从边缘正对着我们,一直到几乎向我们完全展开;与此同时,土星北半球的季节也渐渐地从秋季转变为了冬季。

    地球的黄赤交角是23度,同样土星赤道和土星公转轨道之间有着27度的夹角,这样,就导致了土星和地球一样,总是先让它的一个半球向着太阳,接着是另外的一个半球,如此,就产生了四季的更替。这一系列的图片中的第一张(左下方),拍摄于土星北半球的秋分之后(也就是南半球的春分);位于右上方的最后一张图片,其中我们可以看见土星的倾斜度已经接近最大,则拍摄于北半球的冬至时分(南半球的夏至)。

                   


    为了知道土星光环的颜色和两度方面细微的变化,天文学家们仔细地研究了这些图片。当然他们也想知道到底这光环到底是什么组成的,是怎么形成的,它们到底有多久的历史了。土星的光环不可思议的薄,它的厚度大概只有10米。这些光环是有水结成的冰构成的,它们有的形状很像是一块大石头,或者是小一点的石块。这些石块不断地和别的石头温和地冲撞着,因为他们轨道都是环绕着土星的。而土星的引力场又不时地将一些大的冰块撕裂,以防他们渐渐地积聚起来,形成一个像月亮一样的土星的卫星。我们可以看见的那些光环,呈略带白色的红色,这是因为冰不纯,当中掺有金属元素。

    土星最宽的地方大约有120,000公里。土星的自转速度特别快(土星上的一天相当于地球上的10个小时),这是的土星的极冠部分都变平了。这个巨大的气体星球的地平线上,被强劲的风占领了。而土星上那些精致的颜色的变化,则是由于在大气的上层,有着不少的甲烷,太阳的紫外线照在上面,便形成了这种颜色。在大气的下部,可见的云和气体渐渐变热,而后变成密集的气体,对于探测器来说,这是一个灾难:因为没有陆地可以让它们登陆。

    1997年从地球上发射出去的卡西尼/惠更斯探测器,现在安然无恙的朝着土星系统飞过去。它将于2004年发射一个探测器到泰坦——土星最大的卫星上面去。而后这艘探测器,将绕土星运行四年,以便得到整个土星系统的详细资料。

    由宽视场行星望远镜2号拍摄的这些照片,由Richard French、Jeff Cuzzi、Luke Dones和Jack Lissauer收集了起来,并且赠送给了哈勃Heritage小组。

 

   译自 哈勃网站(http://oposite.stsci.edu

English Title Here
Chinese Version


  Looming like a giant flying saucer in our outer solar system, Saturn puts on a show as the planet and its magnificent ring system nod majestically over the course of its 29-year journey around the Sun. These Hubble Space Telescope images, captured from 1996 to 2000, show Saturn's rings open up from just past edge-on to nearly fully open as it moves from autumn towards winter in its Northern Hemisphere. 
Saturn's equator is tilted relative to its orbit by 27 degrees, very similar to the 23-degree tilt of the Earth. As Saturn moves along its orbit, first one hemisphere, then the other is tilted towards the Sun. This cyclical change causes seasons on Saturn, just as the changing orientation of Earth's tilt causes seasons on our planet. The first image in this sequence, on the lower left, was taken soon after the autumnal equinox in Saturn's Northern Hemisphere (which is the same as the spring equinox in its Southern Hemisphere). By the final image in the sequence, on the upper right, the tilt is nearing its extreme, or winter solstice in the Northern Hemisphere (summer solstice in the Southern Hemisphere). 

  Astronomers are studying this set of images to investigate the detailed variations in the color and brightness of the rings. They hope to learn more about the rings' composition, how they were formed, and how long they might last. Saturn's rings are incredibly thin, with a thickness of only about 30 feet (10 meters). The rings are made of dusty water ice, in the form of boulder-sized and smaller chunks that gently collide with each other as they orbit around Saturn. Saturn's gravitational field constantly disrupts these ice chunks, keeping them spread out and preventing them from combining to form a moon. The rings, as shown here, have a slight pale reddish color due to the presence of organic material mixed with the water ice. 

  Saturn is about 75,000 miles (120,000 km) across, and is flattened at the poles because of its very rapid rotation. A day is only 10 hours long on Saturn. Strong winds account for the horizontal bands in the atmosphere of this giant gas planet. The delicate color variations in the clouds are due to smog in the upper atmosphere, produced when ultraviolet radiation from the Sun shines on methane gas. Deeper in the atmosphere, the visible clouds and gases merge gradually into hotter and denser gases, with no solid surface for visiting spacecraft to land on. 

  The Cassini/Huygens spacecraft, launched from Earth in 1997, is well on its way to the Saturn system. It will arrive in 2004 to land a probe on Titan, Saturn's largest moon, and to orbit the planet for four years for a detailed study of the entire Saturn system. 

  These images of Saturn, taken with the Wide Field Planetary Camera 2 onboard Hubble, were collected by Richard French (Wellesley College), Jeff Cuzzi (NASA/Ames), Luke Dones (SwRI), and Jack Lissauer (NASA/Ames), and have been prepared for presentation by the Hubble Heritage Team. 

 

   From Hubble Web(http://oposite.stsci.edu

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