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卡西尼号成像科学子系统观测到的土星北半球的涡旋(2008 - 2015年)

Vortices in Saturn's Northern Hemisphere (2008-2015) Observed by Cassini ISS.

作者信息

Trammell Harold Justin, Li Liming, Jiang Xun, Pan Yefeng, Smith Mark A, Bering Edgar A, Hörst Sarah M, Vasavada Ashwin R, Ingersoll Andrew P, Janssen Michael A, West Robert A, Porco Carolyn C, Li Cheng, Simon Amy A, Baines Kevin H

机构信息

Department of Earth and Atmospheric Sciences, University of Houston, Houston, Texas, USA.

Department of Physics, University of Houston, Houston, Texas, USA.

出版信息

J Geophys Res Planets. 2016 Sep;121(9):1814-1826. doi: 10.1002/2016JE005122. Epub 2016 Sep 8.

Abstract

We use observations from the Imaging Science Subsystem on Cassini to create maps of Saturn's Northern Hemisphere (NH) from 2008 to 2015, a time period including a seasonal transition (i.e., Spring Equinox in 2009) and the 2010 giant storm. The processed maps are used to investigate vortices in the NH during the period of 2008-2015. All recorded vortices have diameters (east-west) smaller than 6000 km except for the largest vortex that developed from the 2010 giant storm. The largest vortex decreased its diameter from ~11000 km in 2011 to ~5000 km in 2015, and its average diameter is ~6500 km during the period of 2011-2015. The largest vortex lasts at least 4 years, which is much longer than the lifetimes of most vortices (less than 1 year). The largest vortex drifts to north, which can be explained by the beta drift effect. The number of vortices displays varying behaviors in the meridional direction, in which the 2010 giant storm significantly affects the generation and development of vortices in the middle latitudes (25-45°N). In the higher latitudes (45-90°N), the number of vortices also displays strong temporal variations. The solar flux and the internal heat do not directly contribute to the vortex activities, leaving the temporal variations of vortices in the higher latitudes (45-90°N) unexplained.

摘要

我们利用卡西尼号成像科学子系统的观测数据,绘制了2008年至2015年土星北半球的地图,这一时期包括一次季节过渡(即2009年春分)和2010年的巨大风暴。处理后的地图用于研究2008 - 2015年期间北半球的涡旋。除了由2010年巨大风暴形成的最大涡旋外,所有记录的涡旋直径(东西向)均小于6000千米。最大涡旋的直径从2011年的约11000千米减小到2015年的约5000千米,在2011 - 2015年期间其平均直径约为6500千米。最大涡旋持续了至少4年,这比大多数涡旋的寿命(不到1年)长得多。最大涡旋向北漂移,这可以用β漂移效应来解释。涡旋数量在经向上表现出不同的行为,其中2010年的巨大风暴显著影响了中纬度(北纬25 - 45°)涡旋的生成和发展。在高纬度(北纬45 - 90°),涡旋数量也表现出强烈的时间变化。太阳通量和内部热量并未直接促成涡旋活动,因此高纬度(北纬45 - 90°)涡旋的时间变化原因不明。

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