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土卫六热带地区的风暴。

Storms in the tropics of Titan.

作者信息

Schaller E L, Roe H G, Schneider T, Brown M E

机构信息

Institute for Astronomy, University of Hawaii, Honolulu, Hawaii 96822, USA.

出版信息

Nature. 2009 Aug 13;460(7257):873-5. doi: 10.1038/nature08193.

Abstract

Methane clouds, lakes and most fluvial features on Saturn's moon Titan have been observed in the moist high latitudes, while the tropics have been nearly devoid of convective clouds and have shown an abundance of wind-carved surface features like dunes. The presence of small-scale channels and dry riverbeds near the equator observed by the Huygens probe at latitudes thought incapable of supporting convection (and thus strong rain) has been suggested to be due to geological seepage or other mechanisms not related to precipitation. Here we report the presence of bright, transient, tropospheric clouds in tropical latitudes. We find that the initial pulse of cloud activity generated planetary waves that instigated cloud activity at other latitudes across Titan that had been cloud-free for at least several years. These observations show that convective pulses at one latitude can trigger short-term convection at other latitudes, even those not generally considered capable of supporting convection, and may also explain the presence of methane-carved rivers and channels near the Huygens landing site.

摘要

在土星卫星土卫六潮湿的高纬度地区观测到了甲烷云、湖泊以及大多数河流特征,而热带地区几乎没有对流云,却呈现出大量风蚀形成的地表特征,如沙丘。惠更斯探测器在被认为无法支持对流(进而不会有强降雨)的纬度区域的赤道附近观测到了小规模河道和干涸河床,有人认为这是由于地质渗漏或其他与降水无关的机制造成的。在此,我们报告在热带纬度地区存在明亮的、短暂的对流层云。我们发现,云活动的初始脉冲产生了行星波,这些行星波在土卫六上其他至少数年无云的纬度区域引发了云活动。这些观测结果表明,一个纬度上的对流脉冲可以触发其他纬度上的短期对流,即使是那些通常被认为无法支持对流的纬度区域,这也可能解释了惠更斯探测器着陆点附近甲烷侵蚀形成的河流和河道的存在。

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