Giant flux ropes observed in the magnetized ionosphere at Venus

نویسندگان

  • T. L. Zhang
  • W. Baumjohann
  • W. L. Teh
  • R. Nakamura
  • C. T. Russell
  • J. G. Luhmann
  • K. H. Glassmeier
  • E. Dubinin
  • H. Y. Wei
  • A. M. Du
  • Q. M. Lu
  • S. Wang
  • M. Balikhin
چکیده

[1] The Venus ionospheric response to solar and solar wind variations is most evident in its magnetic field properties. Early Pioneer Venus observations during the solar maximum revealed that the Venus ionosphere exhibits two magnetic states depending on the solar wind dynamic pressure conditions: magnetized ionosphere with large-scale horizontal magnetic field; or unmagnetized ionosphere with numerous small-scale thin structures, so-called flux ropes. Here we report yet another magnetic state of Venus’ ionosphere, giant flux ropes in the magnetized ionosphere, using Venus Express magnetic field measurements during solar minimum. These giant flux ropes all have strong core fields and diameters of hundreds of kilometers, which is about the vertical dimension of the ionosphere. This finding represents the first observation of these giant flux ropes at Venus. The cause of these giant flux ropes remains unknown and speculative. Citation: Zhang, T. L., et al. (2012), Giant flux ropes observed in the magnetized ionosphere at Venus, Geophys. Res. Lett., 39, L23103, doi:10.1029/2012GL054236.

برای دانلود رایگان متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Comparison study of magnetic flux ropes in the ionospheres of Venus, Mars and Titan

0019-1035/$ see front matter 2009 Elsevier Inc. A doi:10.1016/j.icarus.2009.03.014 * Corresponding author. Address: 6862 Slichter Hal Angeles, 595 Charles E. Young Drive East, Los Angeles E-mail address: [email protected] (H.Y. Wei). Magnetic flux ropes are created in the ionosphere of Venus and Mars during the interaction of the solar wind with their ionospheres and also at Titan during the i...

متن کامل

The solar wind interaction with Venus through the eyes of the Pioneer Venus Orbiter

Venus has no internal magnetic dynamo and thus its ionosphere and hot oxygen exosphere dominate the interaction with the solar wind. The solar wind at 0.72AU has a dynamic pressure that ranges from 4.5 nPa (at solar max) to 6.6 nPa (at solar min), and its flow past the planet produces a shock of typical magnetosonic Mach number 5 at the subsolar point. At solar maximum the pressure in the ionos...

متن کامل

Stationary flux ropes at the southern terminator of Mars

[1] Flux ropes have long been observed in the upper atmosphere of Venus and more recently at Mars. Here we present magnetic field measurements of flux ropes encountered at the southern terminator of Mars by Mars Global Surveyor and compare them to a flux rope model. This allows several parameters of each rope to be inferred. Remarkably similar flux ropes are met repeatedly at the southern termi...

متن کامل

The nightside ionosphere of Venus under varying levels of solar Euv flux

Solar activity varied widely over the 14 year lifetime of the Pioneer Venus Orbiter, and these variations directly affected the properties of the nightside ionosphere. At solar maximum, when solar EUV was largest, the Venus ionosphere was found to extend to highest altitudes and nightward ion transport was the main source of the nightside ionosphere. At solar minimum, nightward ion transport wa...

متن کامل

Whistler-mode Propagation in the Collisional Ionosphere of Venus

Waves identified as whistler-mode waves have been observed in the nightside ionosphere of Venus by the Pioneer Venus Orbiter. These waves are propagating in a collisional, weakly magnetized ionosphere, and it has been argued that as such they should be damped through collisions, and the wave should not retain the characteristics of the whistler-mode because of non-linear modifications to the di...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

عنوان ژورنال:

دوره   شماره 

صفحات  -

تاریخ انتشار 2012