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[LAMOST科普]土星专辑:“卡西尼—惠更斯”土星探测器探索土星

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LAMOST 发表于 2004-7-2 15:37 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区
在成为第一艘进入土星轨道的飞船后,卡西尼发回了这张照片,拍的是阳光照射的土星光环的一部分。
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LAMOST 发表于 2004-7-2 15:38 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区
在这张照片上可以看到土星的A环里有一道弯曲波(右)和密度波。这张照片是卡西尼宇宙飞船在成功地进入土星轨道后用窄角镜头拍摄的,上面显示的是土星光环黑暗或无光的一面。
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LAMOST 发表于 2004-7-2 15:39 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区
这是卡西尼宇宙飞船成功地进入土星轨道后拍摄的一系列照片中的一张,是用窄角镜头拍摄的
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LAMOST 发表于 2004-7-2 15:40 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区
这是卡西尼宇宙飞船成功地进入土星轨道后拍摄的土星F环照片中的一张,是用飞船的窄角镜头拍摄的阳光照射的一面。
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LAMOST 发表于 2004-7-2 15:40 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区
这张照片显示的是土星A环的三道密度波,是卡西尼飞船在成功地进入土星轨道后用窄角镜头拍摄的光环的黑暗或无光的一面。
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LAMOST 发表于 2004-7-2 15:42 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区

土星档案

  土星是太阳系九大行星之一,按离太阳由近及远的次序为第六颗。中国古代称土星为填星或镇星。

  在1781年发现天王星之前,人们曾认为土星是离太阳最远的行星。在望远镜中可以看到土星被一条美丽的光环围绕。土星还有较多的卫星,到1978年为止,已发现并证实的有10个,以后又陆续有人提出新的发现。

  土星在很多方面像木星,如它与木星同属于巨行星,它的体积是地球的745倍,质量是地球的95.18倍。在太阳系九大行星中,土星的大小和质量仅次于木星,占第二位。它像木星一样被色彩斑斓的云带所缭绕,并被较多的卫星所拱卫。它由于快速自转而呈扁球形。赤道半径约为60,000公里。土星的平均密度只有0.70克/厘米立方米,是九大行星中密度最小的。如果把它放在水中,它会浮在水面上。土星的大半径和低密度使其表面的重力加速度和地球表面相近。土星在冲日时的亮度可与天空中最亮的恒星相比。由于光环的平面与土星轨道面不重合,而且光环平面在绕日运动中方向保持不变,所以从地球上看,光环的视面积便不固定,从而使土星的视亮度也发生变化。当土星光环有最大视面积时,土星显得亮一些;当视线正好与光环平面重合时,光环便呈现为一条直线,土星就显得暗些。二者之间的亮度大约相差3倍。

  土星绕太阳公转的轨道半径约为14亿公里,它的轨道是椭圆的。它同太阳的距离在近日点时和在远日点时相差约1 .5亿公里。土星绕太阳公转的平均速度约为每秒9.64公里,公转一周约29.5年。土星也有四季,只是每一季的时间要长达7年多,因为离太阳遥远,既使是夏季也十极其寒冷。土星自转很快,但不同纬度自转的速度却不一样,这种差别比木星还大。赤道上自转周期是10小时14分,纬度60度处则变成10小时40分。这就是说在土星赤道上,一个昼夜只有10小时零14分。

  土星大气以氢、氦为主,并含有甲烷和其他气体,大气中飘浮着由稠密的氨晶体组成的云。从望远镜中看去,这些云像木星的云一样形成相互平行的条纹,但不如木星云带那样鲜艳,只是比木星云带规则得多。土星云带以金黄色为主,其余是桔黄色、淡黄色等。土星的表面同木星一样,也是流体的。它赤道附近的气流与自转方向相同,速度可达每秒500米,比木星上的风力要大得多。

  土星极地附近呈绿色,是整个表面最暗的区域。根据红外观测得知,云顶温度为-170℃,比木星低50℃。土星表面的温度约为-140℃。土星表面有时会出现白斑,最著名的白斑是1933年8月发现的,这块白斑出现在赤道区,呈蛋形,长度达到土星直径的1/5。以后这个白斑不断地扩大,几乎蔓延到整个赤道带。

  由于这颗行星表面温度较低而逃逸速度又大(35.6公里/秒),使土星保留着几十亿年前它形成时所拥有的全部氢和氦。因此,科学家认为,研究土星目前的成分就等于研究太阳系形成初期的原始成分,这对于了解太阳内部活动及其演化有很大帮助。一般认为土星的化学组成像木星,不过氢的含量较少。土星上的甲烷含量比木星多,而氨的含量则比木星少。

  1973年 4月美国发射的行星际探测器“先驱者”11号发现土星有一个由电离氢构成的广延电离层,其高层温度约为977℃。观测结果表明,土星极区有极光。

  目前认为,土星形成时,起先是土物质和冰物质吸积,继之是气体积聚。因此,土星有一个直径20,000公里的岩石核心。这个核占土星质量的10%到20%,核外包围着5,000公里厚的冰壳,再外面是8,000公里厚的金属氢层,金属氢之外是一个广延的分子氢层。

  1969年,一架飞机在地球大气高层对土星的热辐射作了红外观测,发现土星和木星一样,它辐射出的能量是它从太阳接收到的能量的两倍。这表明土星和木星一样有内在能源。后来“先驱者”11号的红外探测证实了这一点,测得土星发出的能量是从太阳吸收到的2.5倍。

  1610年,意大利天文学家伽利略观测到在土星的球状本体旁有奇怪的附属物。1659年,荷兰学者惠更斯证认出这是离开本体的光环。1675年意大利天文学家卡西尼,发现土星光环中间有一条暗缝,后称卡西尼环缝。他还猜测,光环是由无数小颗粒构成。两个多世纪后的分光观测证实了他的猜测。但在这二百年间,土星环通常被看作是一个或几个扁平的固体物质盘。直到1856年,英国物理学家麦克斯韦从理论上论证了土星环是无数个小卫星在土星赤道面上绕土星旋转的物质系统。(关于行星环)

  土星环位于土星的赤道面上。在空间探测以前,从地面观测得知土星环有五个,其中包括三个主环(A环、B环、C环)和两个暗环(D环、E环)。B环既宽又亮,它的内侧是C环,外侧是A环。A环和B环之间为宽约5,000公里的卡西尼缝,它是天文学家卡西尼在1675年发现的。B环的内半径 91,500公里,外半径116,500公里,宽度是25,000公里,可以并排安放两个地球。A环的内半径121,500公里,外半径137,000公里,宽度15,500公里。C环很暗,它从B环的内边缘一直延伸到离土星表面只有12,000公里处,宽度约19,000公里。1969年在C环内侧发现了更暗的D环,它几乎触及土星表面。在A环外侧还有一个E环,由非常稀疏的物质碎片构成,延伸在五、六个土星半径以外。1979年9月,“先驱者” 11号探测到两个新环──F环和G环。F环很窄,宽度不到800公里,离土星中心的距离为2.33个土星半径,正好在A环的外侧。G环离土星很远,展布在离土星中心大约10~15个土星半径间的广阔地带。“先驱者”11号还测定了A环、B环、C环和卡西尼缝的位置、宽度,其结果同地面观测相差不大。“先驱者”11号的紫外辉光观测发现,在土星的可见环周围有巨大的氢云。环本身是氢云的源。

  除了A环、B环、C 环以外的其他环都很暗弱。土星的赤道面与轨道面的倾角较大,从地球上看,土星呈现出南北方向的摆动,这就造成了土星环形状的周期变化。仔细观测发现,土星环内除卡西尼缝以外,还有若干条缝,它们是质点密度较小的区域,但大多不完整且具有暂时性。只有A环中的恩克缝是永久性的,不过,环缝也不完整。科学家认为这些环缝都是土星卫星的引力共振造成的,犹如木星的巨大引力摄动造成小行星带中的柯克伍德缝一样。“先驱者”11号在A环与F环之间发现一个新的环缝,称为“先驱者缝”,还测得恩克缝的宽度为876公里。由观测阐明土星环的本质,要归功于美国天文学家基勒,他在1895年从土星环的反射光的多普勒频移发现土星环不是固体盘,而是以独立轨道绕土星旋转的大群质点。土星环掩星并没有把被掩的星光完全挡住,这也说明土星环是由分离质点构成的。1972年从土星环反射的雷达回波得知,环的质点是直径介于4到30厘米之间的冰块。
我的新BLOG家:http://waynelamost.spaces.live.com摄影小站:http://lamost423.blog.sohu.com/相册:http://photo.163.com/photos/lamost423/http://i.cn.yahoo.com/lamost423
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LAMOST 发表于 2004-7-2 15:45 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区

Titan[土卫六]

土卫六是土星的已知卫星中距其第十五近的一颗:

公转轨道: 距土星 1,221,830 千米
卫星直径: 5150 千米
质量: 1.35e23 千克
在希腊神话里,泰坦是一个巨人家族,乌拉诺斯和该亚的孩子。他想支配天堂,但是被宙斯家族推翻并取代了。

   它是在1655年由惠更斯发现的。

   人们一直认为土卫六是太阳系中最大的卫星,但最近的观察表明土卫六的大气层太厚了,其实它的固体表面比木卫三的还稍小一些。尽管如此,土卫六还是在直径上比水星大,并且比冥王星更大更重。

   旅行者1号任务的根本目的之一是对土卫六的研究。旅行者1号在距其表面4000千米的高空飞行。我们现在与它邂逅的几分钟比先前的300年了解的更多。

   现在我们所知道的还很不完整。土卫六被一个很圆的不透明大气层所包围,其表面在可见光下根本看不见(左下图)。(卡西尼任务将用雷达绘制土卫六表面的地图,就象Magellan对金星所做的。)所有旅行者的图片显示的是在南北半球颜色上的微妙变化,一些地表的细节可以用哈博太空望远镜通过红外线被看见。

   土卫六的整体性质与木卫三,木卫四,海卫一和冥王星(可能)相类似。现在还不知道它是类似木卫三的内部构造还是与木卫四相同。

   土卫六是由近一半的冰和一半的岩石物质组成的。它可能被分成许多层,拥有一个直径3400千米,被许多由多种冰晶体组成的地层环绕的岩石核心。它的内部可能还是热的,尽管在组成上与土卫五和其余的土星卫星类似,但是它密度更大,因为它很大以致于自身的引力使它向中心压缩。

   在太阳系的所有卫星中,土卫六有一个值得注意的大气层。在地表,它的压力大于1.5巴(比地球的高50%)。它主要由分子氮组成(就像地球的),另外仅有6%的氩气和占有一些百分比的甲烷。十分有趣的是,还有一打微量的其他有机化合物(比如乙烷,氢氰酸,二氧化碳)。这些有机物像甲烷一样形成。它们在土卫六的大气层上部被太阳光破坏。这样的结果是类似于在大城市上空发现的烟雾,但要更厚。在许多方面,这类似于地球历史上生命开始出现的早期的条件。

   土卫六没有磁场,有时在土星的磁层外运行,这就直接暴露在了太阳风下。这可能造成电离,并从大气层的顶部带走一些分子。

   在表面,土卫六的温度是大约94开(零下290华氏度)。在这个温度下,冰不会升华,表面的水不能参与大气层的化学变化。尽管如此,好像还有许多化学变化不断进行;这最终的结果可能形成许多很厚的烟雾。

   可能有两个云层在大约200和300千米的上空。其他的一些少量的复杂的化学变化一定是引起从宇宙中看到它为枯黄色的原因。

   似乎可能由乙烷组成的云能产生一种液态乙烷的雨落到表面,可能形成一个乙烷组成的“大洋”(或是乙烷和甲烷混合),有1000米那么深。然而,最近对表面的雷达观察已经对此产生怀疑。

   
   通过哈博天文望远镜的观察也显示土卫六的自转实际上是像大多数土星卫星一样的,为同步自转。
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LAMOST 发表于 2004-7-2 15:46 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区
Titan
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LAMOST 发表于 2004-7-2 15:48 | 显示全部楼层 来自: 中国–天津–天津 联通/天奕网吧

土卫六的未知

未知点
表面是否有液体?
内部是否还是热的?
为什么土卫六拥有一个稠密的大气层而其他的大卫星却没有?
在土卫六上有许多有机化合物和可能潜在的液体环境。尽管它对于生命来说极其寒冷,但是否有存在的可能?土卫六是最有可能有生命的星球之一。不管怎样,有趣的是,它类似于地球早期的环境。
卡西尼雷达绘图器和惠更斯探测器会提供强有力的数据来弥补人们因对此谜一般的卫星了解的缺乏而产生的灰心。(如果它的议案能幸运地被美国国会通过。)
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LAMOST 发表于 2004-7-2 15:52 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区

土卫九

6月23日,美国宇航局发布了一张由“卡西尼”号飞船拍摄的土卫九表面照片。
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LAMOST 发表于 2004-7-2 15:53 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区
美国宇航局6月15日公布的土星外围最大卫星——土卫九的照片。土星探测飞船“卡西尼”号11日近距离掠过土卫九,并成功拍摄到迄今最好的土卫九照片。清晰的图像显示,土卫九与彗星有点相像,表面有冰,并覆盖着灰土。
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LAMOST 发表于 2004-7-2 15:54 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区
国宇航局6月15日公布的
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LAMOST 发表于 2004-7-2 15:55 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区
美国宇航局6月15日公布
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LAMOST 发表于 2004-7-2 15:57 | 显示全部楼层 来自: 中国–天津–天津 广电网/福中网吧B区
土卫九的真实形状
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LAMOST 发表于 2004-7-4 14:58 | 显示全部楼层 来自: 中国–天津–天津 联通

Two-Tone Titan

Two-Tone Titan
Original Caption Released with Image:
Cassini's finely-tuned vision reveals hazes high in the skies over Titan in this narrow angle camera image taken by the Cassini spacecraft on May 22, 2004. Here the northern hemisphere is notably brighter than the southern hemisphere. This trait was noticed in images returned by the Voyager spacecraft, but the effect is presently reversed, North to South, as Titan is currently experiencing opposite seasons from those during the Voyager epoch 23 years ago.

The image was taken from a distance of 21.7 million kilometers (13.5 million miles) from Saturn through a filter sensitive to strong absorption by methane gas (centered at 889 nanometers). The image scale is 129 kilometers (80 miles) per pixel.

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Cassini-Huygens mission for NASA's Office of Space Science, Washington, D.C. The Cassini orbiter and its two onboard cameras, were designed, developed and assembled at JPL. The imaging team is based at the Space Science Institute, Boulder, Colo.

For more information, about the Cassini-Huygens mission visit, http://saturn.jpl.nasa.gov and the Cassini imaging team home page, http://ciclops.org.



Image Credit:
NASA/JPL/Space Science Institute



--------------------------------------------------------------------------------

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Target Name: Titan
Is a satellite of: Saturn
Mission: Cassini

Spacecraft: Cassini Orbiter

Instrument: Imaging Science Subsystem - Narrow Angle

Product Size: 640 samples x 640 lines
Produced By: CICLOPS/Space Science Institute

Primary Data Set: Cassini
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LAMOST 发表于 2004-7-4 15:04 | 显示全部楼层 来自: 中国–天津–天津 联通

Titan’s thick haze layer

Original Caption Released with Image:
Titan's thick haze layer is shown in this enhanced Voyager 1 image taken Nov. 12, 1980 at a distance of 435,000 kilometers (270,000 miles). Voyager images of Saturn's largest moon show Titan completely enveloped by haze that merges with a darker "hood" or cloud layer over the north pole. Such a mantle is not present at the south pole. At Voyager's closest approach to Titan on Nov. 11, 1980, spacecraft instruments found that the moon has a substantial atmosphere, far denser than that of Mars and possibly denser than Earth's. The Voyager Project is managed for NASA by the Jet Propulsion Laboratory, Pasadena, Calif.


Target Name: Titan
Is a satellite of: Saturn
Mission: Voyager

Spacecraft: Voyager 1

Instrument: Imaging Science Subsystem - Narrow Angle

Product Size: 485 samples x 580 lines
Produced By: JPL

Producer ID: P23108

Addition Date: 2000-03-16
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LAMOST 发表于 2004-7-4 15:08 | 显示全部楼层 来自: 中国–天津–天津 联通
Original Caption Released with Image:
This Voyager 2 photograph of Titan, taken Aug. 23 from a range of 2.3 million kilometers (1.4 million miles), shows some detail in the cloud systems on this Saturnian moon. The southern hemisphere appears lighter in contrast, a well-defined band is seen near the equator, and a dark collar is evident at the north pole. All these bands are associated with cloud circulation in Titan's atmosphere. The extended haze, composed of submicron-size particles, is seen clearly around the satellite's limb. This image was composed from blue, green and violet frames.
JPL manages the Voyager project for NASA's Office of Space Science.


Target Name: Titan
Is a satellite of: Saturn
Mission: Voyager

Spacecraft: Voyager 2

Product Size: 1296 samples x 960 lines
Produced By: JPL

Producer ID: P24067

Addition Date: 1999-05-08
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LAMOST 发表于 2004-7-4 15:14 | 显示全部楼层 来自: 中国–天津–天津 联通
Original Caption Released with Image:
Layers of haze covering Saturn's satellite Titan are seen in this image taken by Voyager 1 on Nov. 12, 1980 at a range of 22,000 kilometers (13,700 miles). The colors are false and are used to show details of the haze that covers Titan. The upper level of the thick aerosol above the satellite's limb appears orange. The divisions in the haze occur at altitudes of 200, 375 and 500 kilometers (124, 233 and 310 miles) above the limb of the moon.
JPL manages the Voyager project for NASA's Office of Space Science.


Target Name: Titan
Is a satellite of: Saturn
Mission: Voyager

Spacecraft: Voyager 1

Product Size: 1715 samples x 1825 lines
Produced By: JPL

Producer ID: P23107

Addition Date: 1999-05-08
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LAMOST 发表于 2004-7-4 15:47 | 显示全部楼层 来自: 中国–天津–天津 联通
Original Caption Released with Image:
Voyager 2 obtained this wide-angle image of the night side of Titan on Aug. 25 at a high phase angle of 154` and a range of 907,000 kilometers (563,000 miles). Green and violet images were combined to make this photograph. The result is a view of the extended atmosphere of this satellite of Saturn, the bright orangish ring being caused by the atmosphere's scattering of the incident sunlight. The bluish outer ring is further evidence of scattering by the submicron size particles that extend several hundred kilometers above the main clouds. This type of photograph is a direct indication of Titan's extensive atmosphere. The Voyager project is managed for NASA by the Jet Propulsion Laboratory, Pasadena.

Image Note:
Green - PICNO 1244S2-001Red - PICNO 1244S2-001Blue - PICNO 1250S2-001
Target Name: Titan
Is a satellite of: Saturn
Mission: Voyager

Spacecraft: Voyager 2

Instrument: Imaging Science Subsystem - Narrow Angle

Product Size: 200 samples x 200 lines
Produced By: JPL

Producer ID: P23949

Addition Date: 1999-02-23
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LAMOST 发表于 2004-7-4 15:51 | 显示全部楼层 来自: 中国–天津–天津 联通
Original Caption Released with Image:
Scientists for the first time have made images of the surface of Saturn's giant, haze-shrouded moon, Titan. They mapped light and dark features over the surface of the satellite during nearly a complete 16-day rotation. One prominent bright area they discovered is a surface feature 2,500 miles across, about the size of the continent of Australia.
Titan, larger than Mercury and slightly smaller than Mars, is the only body in the solar system, other than Earth, that may have oceans and rainfall on its surface, albeit oceans and rain of ethane-methane rather than water. Scientists suspect that Titan's present environment -- although colder than minus 289 degrees Fahrenheit, so cold that water ice would be as hard as granite -- might be similar to that on Earth billions of years ago, before life began pumping oxygen into the atmosphere.

Peter H. Smith of the University of Arizona Lunar and Planetary Laboratory and his team took the images with the Hubble Space Telescope during 14 observing runs between Oct. 4 - 18. Smith announced the team's first results last week at the 26th annual meeting of the American Astronomical Society Division for Planetary Sciences in Bethesda, Md. Co-investigators on the team are Mark Lemmon, a doctoral candidate with the UA Lunar and Planetary Laboratory; John Caldwell of York University, Canada; Larry Sromovsky of the University of Wisconsin; and Michael Allison of the Goddard Institute for Space Studies, New York City.

Titan's atmosphere, about four times as dense as Earth's atmosphere, is primarily nitrogen laced with such poisonous substances as methane and ethane. This thick, orange, hydrocarbon haze was impenetrable to cameras aboard the Pioneer and Voyager spacecraft that flew by the Saturn system in the late 1970s and early 1980s. The haze is formed as methane in the atmosphere is destroyed by sunlight. The hydrocarbons produced by this methane destruction form a smog similar to that found over large cities, but is much thicker.

Smith's group used the Hubble Space Telescope's WideField/Planetary Camera 2 at near-infrared wavelengths (between .85 and 1.05 microns). Titan's haze is transparent enough in this wavelength range to allow mapping of surface features according to their reflectivity. Only Titan's polar regions could not be mapped this way, due to the telescope's viewing angle of the poles and the thick haze near the edge of the disk. Their image-resolution (that is, the smallest distance seen in detail) with the WFPC2 at the near-infrared wavelength is 360 miles. The 14 images processed and compiled into the Titan surface map were as "noise" free, or as free of signal interference, as the space telescope allows, Smith said.

Titan makes one complete orbit around Saturn in 16 days, roughly the duration of the imaging project. Scientists have suspected that Titan's rotation also takes 16 days, so that the same hemisphere of Titan always faces Saturn, just as the same hemisphere of the Earth's moon always faces the Earth. Recent observations by Lemmon and colleagues at the University of Arizona confirm this true.

It's too soon to conclude much about what the dark and bright areas in the Hubble Space Telescope images are -- continents, oceans, impact craters or other features, Smith said. Scientists have long suspected that Titan's surface was covered with a global ehtane-methane ocean. The new images show that there is at least some solid surface.

Smith's team made a total 50 images of Titan last month in their program, a project to search for small scale features in Titan's lower atmosphere and surface. They have yet to analyze images for information about Titan's clouds and winds. That analysis could help explain if the bright areas are major impact craters in the frozen water ice-and-rock or higher-altitude features.

The images are important information for the Cassini mission, which is to launch a robotic spacecraft on a 7-year journey to Saturn in October 1997. About three weeks before Cassini's first flyby of Titan, the spacecraft is to release the European Space Agency's Huygens Probe to parachute to Titan's surface. Images like Smith's team has taken of Titan can be used to identify choice landing spots - - and help engineers and scientists understand how Titan's winds will blow the parachute through the satellite's atmosphere.

UA scientists play major roles in the Cassini mission: Carolyn C. Porco, an associate professor at the Lunar and Planetary Laboratory, leads the 14-member Cassini Imaging Team. Jonathan I. Lunine, also an associate professor at the lab, is the only American selected by the European Space Agency to be on the three-member Huygens Probe interdisciplinary science team. Smith is a member of research professor Martin G. Tomasko's international team of scientists who will image the surface of Titan in visible light and in color with the Descent Imager/Spectral Radiometer, one of five instruments in the Huygens Probe's French, German, Italian and U.S. experiment payload. Senior research associate Lyn R. Doose is also on Tomasko's team. Lunine and LPL professor Donald M. Hunten are members of the science team for another U.S. instrument on that payload, the gas chromatograph mass spectrometer. Hunten was on the original Cassini mission science definition team back in 1983.

PHOTO CAPTION: Four global projections of the HST Titan data, separated in longitude by 90 degrees. Upper left: hemisphere facing Saturn. Upper right: leading hemisphere (brightest region). Lower left: the hemisphere which never faces Saturn. Lower right: trailing hemisphere. Not that these assignments assume that the rotation is synchronous. The imaging team says its data strongly support this assumption -- a longer time baseline is needed for proof. The surface near the poles is never visible to an observer in Titan's equatorial plane because of the large optical path.

The Wide Field/Planetary Camera 2 was developed by the Jet Propulsion Laboratory and managed by the Goddard Spaced Flight Center for NASA's Office of Space Science.

This image and other images and data received from the Hubble Space Telescope are posted on the World Wide Web on the Space Telescope Science Institute home page at URL http://oposite.stsci.edu/pubinfo/


Image Note:
Credit: Peter H. Smith and Mark Lemmon of the UA Lunar and Planetary Laboratory, and NASA
Target Name: Titan
Is a satellite of: Saturn
Mission: Hubble Space Telescope (HST)

Spacecraft: Hubble Space Telescope

Instrument: Wide Field Planetary Camera 2

Product Size: 600 samples x 750 lines
Produced By: Space Telescope Science Institute

Producer ID: STSCI-PRC94-55

Addition Date: 1998-09-26
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